faraday's first dynamo: a retrospective
TRANSCRIPT
Faradays first dynamo A retrospectiveGlenn S Smith
Citation American Journal of Physics 81 907 (2013) doi 10111914825232 View online httpdxdoiorg10111914825232 View Table of Contents httpscitationaiporgcontentaaptjournalajp8112ver=pdfcov Published by the American Association of Physics Teachers Articles you may be interested in Hands-on Experiments on Faradays Law Phys Teach 43 228 (2005) 10111911888083 An experimental observation of Faradayrsquos law of induction Am J Phys 70 595 (2002) 10111911405504 Unconventional Dynamo Phys Teach 40 220 (2002) 10111911474144 Only the integral form of the law of electromagnetic induction explains the dynamo Am J Phys 66 543 (1998) 101119118903 Some rigorous results for the kinematic dynamo problem with general boundary conditions J Math Phys 38 1583 (1997) 1010631531817
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Faradayrsquos first dynamo A retrospective
Glenn S Smitha)
School of Electrical and Computer Engineering Georgia Institute of Technology AtlantaGeorgia 30332-0250
(Received 28 June 2013 accepted 2 October 2013)
In the early 1830s Michael Faraday performed his seminal experimental research on
electromagnetic induction in which he created the first electric dynamomdasha machine for
continuously converting rotational mechanical energy into electrical energy His machine was a
conducting disc rotating between the poles of a permanent magnet with the voltagecurrent
obtained from brushes contacting the disc In his first dynamo the magnetic field was asymmetric
with respect to the axis of the disc This is to be contrasted with some of his later symmetric
designs which are the ones almost invariably discussed in textbooks on electromagnetism In this
paper a theoretical analysis is developed for Faradayrsquos first dynamo From this analysis the eddy
currents in the disc and the open-circuit voltage for arbitrary positioning of the brushes are
determined The approximate analysis is verified by comparing theoretical results with
measurements made on an experimental recreation of the dynamo Quantitative results from the
analysis are used to elucidate Faradayrsquos qualitative observations from which he learned so much
about electromagnetic induction For the asymmetric design the eddy currents in the disc
dissipate energy that makes the dynamo inefficient prohibiting its use as a practical generator of
electric power Faradayrsquos experiments with his first dynamo provided valuable insight into
electromagnetic induction and this insight was quickly used by others to design practical
generators VC 2013 American Association of Physics Teachers
[httpdxdoiorg10111914825232]
I INTRODUCTION
In 1831 Michael Faraday (Fig 1) embarked on one of themost productive periods of his career during which heexperimented with electromagnetism and among otherthings discovered electromagnetic induction Faraday wasaware of research that had been done earlier on theContinent in particular the experiments on magnetism of theFrench scientist Francois Arago In 1824 Arago discovered aphenomenon that would become known as ldquoAragorsquosrotationsrdquo1 Arago suspended a magnetized needle parallel toand above a copper disc When he rotated the disc about itsaxis he noticed that the needle also rotated in the samedirection as the disc At the time there was much speculationas to the cause of these rotations In his ExperimentalResearches in Electricity Faraday commented that ldquohellipIhope to make the experiment of Arago a new source of elec-tricityhelliprdquo and this he did in his subsequent research2
Faraday invented the first electric dynamosmdashmachines forcontinuously converting rotational mechanical energy intoelectrical energy
Figure 2(a) shows a sketch of Faradayrsquos first dynamo Thissketch is based on a drawing from Faradayrsquos diary datedOctober 28 183134 Probably because of his familiarity withAragorsquos experiment Faraday chose to use a copper discmounted on an axle in his experiment He placed the discbetween the poles of a strong permanent magnet and heused mercury-coated sliding contacts to connect the disc toan external circuit containing a simple but sensitive galva-nometer Faraday called these contacts ldquoelectric collectorsrdquobut we would now call them ldquobrushesrdquo As Faraday rotatedthe disc he observed a continuous deflection of the galva-nometer Faraday performed many experiments with thisdynamo in an effort to understand the physics of electromag-netic induction We will have more to say about these experi-ments later in this paper
After studying his first dynamo Faraday examined otherconfigurations for the dynamo one of which is shown in Fig2(b) This sketch is based on a drawing from SilvanusThompsonrsquos biography of Faraday and the dynamo is dis-cussed in an entry in Faradayrsquos diary dated December 1618315ndash7 Faraday cut a circular hole of slightly bigger
Fig 1 Portrait of Michael Faraday (ca 1840s) taken sometime after the
publication of the first volume of his Experimental Researches inElectricity in which he describes his early dynamos Smithsonian Institution
Archives Image SIA2012-1087
907 Am J Phys 81 (12) December 2013 httpaaptorgajp VC 2013 American Association of Physics Teachers 907
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diameter than his disc in a lead sheet then he placed the cop-per disc in the hole and filled the space between the disc andsheet with mercury He fastened one lead from his galva-nometer to the sheet and placed the other lead in a mercury-filled cup atop the axle of the disc The magnetic field wasthe Earthrsquos which has a significant component normal to thesurface of the Earth in London hence normal to the horizon-tal disc As Faraday rotated the disc he observed a deflectionof the galvanometer Notice that unlike Faradayrsquos firstdynamo all of the components of this dynamo (the disc thebrush formed by the mercury-filled trough and the compo-nent of the magnetic field normal to the disc) are rotationallysymmetric about the axis of the disc
Most textbooks on electromagnetism contain a discussion orproblem involving a symmetrical dynamo which in almost allrespects is the same as Faradayrsquos design in Fig 2(b) Sometimesit is referred to as a ldquounipolar generatorrdquo or a ldquohomopolar gener-atorrdquo Because of the simplicity of the symmetrical structure asolution for the open-circuit voltage V at the terminals A-B iseasily found by a few different methods to be
V frac14 xB0A2
2 (1)
where A and x are the radius and the angular frequency forthe disc and B0 is the component of the applied magneticfield that is normal to the disc Experimental results that ver-ify Eq (1) have been presented in a number of papers8ndash12
and more detailed discussions of the symmetrical dynamoare in the books of Woodson and Melcher and Van Bladeland in the papers of Van Bladel and Montgomery13ndash16
Faradayrsquos first dynamo the asymmetric one shown in Fig2(a) has received much less attention There is no mentionof it in most textbooks on electromagnetism In a paper from1942 and later in the third edition of his graduate-level text-book William Smythe analyzed a geometry similar toFaradayrsquos but he did not discuss it in the context of adynamo for example he did not determine the open-circuitvoltage1718
The purpose of this paper is to present a detailed discussionof Faradayrsquos first dynamo supported by new analytical and ex-perimental results This material particularly the graphicscan be used to present the historically important story ofFaradayrsquos accomplishments to students in undergraduate andgraduate courses in electromagnetism In Sec II we describean analysis of the dynamo in which Smythersquos approximateresult for the magnetic scalar potential is used to obtain thecurrent in the disc and we extend this result to include theopen-circuit voltage for all points on the disc In Sec III wepresent quantitative numerical results from the analysis andshow how these results are related to Faradayrsquos qualitativeobservations In Sec IV we describe an experiment that issimilar to Faradayrsquos but based on modern materials and instru-mentation Measurements from this experiment validate theapproximate analysis Finally Sec V contains a discussion inwhich we address the question ldquoWhat ever became ofFaradayrsquos first dynamordquo or stated differently ldquoHow is hismachine used todayrdquo
II ANALYSIS OF FARADAYrsquoS FIRST DYNAMO
The analysis for the dynamo is based on the model shownin Fig 3(a) the coordinates and dimensions are on the planview of the disc in Fig 3(b) The circular disc of radius Aand thickness d has electrical conductivity r permeabilityl0 and rotates with angular frequency x The applied axialmagnetic field ~Ba frac14 B0z is uniform over the circular area ofradius a located at a distance c from the axis of the disc(gray area in the figure) The external circuit formed fromperfectly conducting wire makes contact with the disc at thebrush on the axis (C) and at the brush at the point ethqbubTHORN onthe disc (D) The open-circuit voltage V is determined at theterminals A-B in the external circuit The analysis is per-formed in the laboratory frame which is the frame in whichthe magnet and the external circuit are at rest The electro-magnetic field is time-invariant in this frame because of therotational symmetry of the disc To see this consider whathappens when a hole is cut into the disc destroying the rota-tional symmetry The electromagnetic field in the laboratoryframe is then a periodic function of time
The analysis is a quasi-static one in which magneticeffects are assumed to be dominant and all dimensions areelectrically small so that any retardation in time for the fieldcan be ignored19 In Maxwellrsquos equations the displacementcurrent ~D=t and the volume charge density q are ignoredThe latter condition means that any convection current dueto the motion of free charge is also ignored In addition tothe applied magnetic field ~Ba there is the magnetic field ~Bi
Fig 2 (a) Faradayrsquos first dynamo based on a drawing from Faradayrsquos di-
ary3 (b) One of Faradayrsquos rotationally symmetric configurations for a
dynamo based on a drawing by Thompson5
908 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 908
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13023920174 On Sun 24 Aug 2014 212302
due to the current induced in the disc In the source-freeregion outside the disc the two Maxwellrsquos equations thatinvolve the magnetic field ~Bi are
r ~Bi frac14 0 (2)
and
r ~Bi 0 (3)
The volume density for the conduction current ~J is assumedto be uniform throughout the thickness of the disc with anegligible axial component Thus it can be approximated bya surface- or sheet-current density ~Js ~Jd20
The boundary condition that relates the surface currentdensity to the magnetic field is
~JsethquTHORN frac141
l0
z frac12~Biethqu z frac14 0thornTHORN ~Biethqu z frac14 0THORN
frac14 2
l0
z ~Biethqu z frac14 0thornTHORN (4)
where for the last term we have used the fact that the compo-nent of the magnetic field tangential to the surface of the dischas odd symmetry about the disc as shown in Fig 4(a)
A Magnetic scalar potential
We can represent the irrotational magnetic field Bi by ascalar magnetic potential U via21
~Bi frac14 rU (5)
This is inserted into Eq (2) to obtain Laplacersquos equation forthe potential in a source-free region
r2U frac14 0 (6)
For describing the potential at the top surface of the disc(zfrac14 0thorn) we will define the three regions on the disc shownin Fig 5 The two radial lines at ua frac14 6sin1etha=cTHORN are tan-gent to the boundary of the circular region containing theapplied magnetic field Region I (light gray) is bounded bythese lines (ua u ua) and is above the applied mag-netic field qo lt q A with qo frac14 cfrac12cosu
thornffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region II (dark gray) is within the
applied magnetic field ua u ua and qi q qo
with qi frac14 cfrac12cosuffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region III (white) is
everywhere else on the disc Using this notation the appliedmagnetic field can be expressed as
~BaethquTHORN frac14 BaethquTHORNzfrac14 B0fUfrac12q qiethuTHORN Ufrac12q qoethuTHORNgfrac12Uethuthorn uaTHORN Uethu uaTHORNz (7)
in which U(n) is the Heaviside unit-step function
Fig 3 (a) Model used in the analysis of the dynamo (b) Plan view of the
disc showing the coordinates and dimensions
Fig 4 Details for the surface current in the disc (a) Boundary condition
relating the magnetic field to the surface current density (b) Tube of surface
current showing coordinates
909 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 909
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13023920174 On Sun 24 Aug 2014 212302
Smythe gives approximate expressions for the magnetic scalar potential in these regions as171822
UIethqnu z frac14 0thornTHORN frac14 UIIIethqnu z frac14 0thornTHORN frac14 xB0Acrd
2a2
nqnsinu1
q2n thorn c2
n 2cnqncosu 1
c2nq
2n thorn 1 2cnqncosu
(8)
and
UIIethqnu z frac14 0thornTHORN
frac14 xB0Acrd
2qnsinu 1 a2
n
c2nq
2n thorn 1 2cnqncosu
(9)
in which we have normalized the dimensions to the radius ofthe disc that is qn frac14 q=A an frac14 a=A etc
Figure 6 is a contour plot of the scalar potential normal-ized so that maxjUnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 These parameters are roughly the same as thoseused for the experiments described later All of the contoursare spaced by the increment Un frac14 01 except the incom-plete contours for Un frac14 6001 and 6 005 Notice that thepotential has odd symmetry about the line u frac14 0 180
(positive on the left and negative on the right) and the poten-tial is zero along that line and along the edge of the discwhere qfrac14A
B Surface current density
We are generally more used to interpreting the surfacecurrent density than the magnetic scalar potential and theformer is easily obtained from the latter Inserting Eq (5)into Eq (4) we obtain
~JsethquTHORN frac14 2
l0
z r2Uethqu z frac14 0thornTHORN (10)
where we have use r2 to indicate that the gradient is onlywith respect to the two variables q u
The equipotential lines (Ufrac14 constant) such as those inFig 6 are also streamlines of the surface current densitythat is at every point along one of these lines the surface cur-rent is tangential to the line To show this we first note thatr2U is normal to the equipotential lines The operation
r2U ~Js frac14 2
lo
r2U ethz r2UTHORN
frac14 2
lo
z ethr2Ur2UTHORN frac14 0 (11)
shows that the surface current density is normal to r2UHence the surface current is parallel or tangential to theequipotential lines
Two adjacent equipotential lines such as the lines for U1
and U2 in Fig 4(b) bound a two-dimensional tube of surfacecurrent23 At any cross section of the tube the total current Ithrough the tube is the same To show this we first recallfrom Eq (3) that the magnetic field is irrotational so in anyregion in which the field is well defined the line integral of~Bi between two points such as from P1 to P2 in Fig 4(b) isindependent of the path of integration21 Thus
ethP2
P1
~Bi t dlsquo frac14 ethP2
P1
r2U t dlsquo frac14 ethU2 U1THORN (12)
Fig 5 Regions and coordinates used in the description of the scalar mag-
netic potential U at the top surface (zfrac14 0thorn) of the disc
Fig 6 Contour plot for the magnetic scalar potential Unethqu z frac14 0thornTHORN for
the case aAfrac14 0170 and cAfrac14 0667 The potential is normalized so that
maxjUnj frac14 10 and the contours are spaced by the increment Un frac14 01
except the incomplete contours for Unfrac146001 and 6005 The equipoten-
tial lines are also streamlines of the surface current density and the arrows
on these lines show the direction of the current Two adjacent equipotential
lines bound a tube of surface current through which the total current I is the
same at any cross section
910 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 910
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13023920174 On Sun 24 Aug 2014 212302
where t is a unit vector tangent to the path After taking frac12zEq (4) t and rearranging terms we obtain
~Bi t frac14 l0
2ethz ~JsTHORN t (13)
Substituting Eq (13) into the left-hand side of Eq (12) gives
l0
2
ethP2
P1
ethz ~JsTHORN t dlsquo frac14 l0
2
ethP2
P1
~Js s dlsquo frac14 ethU2 U1THORN
(14)
in which the unit vector s frac14 z t is in the plane of the discand normal to the path as shown in Fig 4(b) Now from Eq(14) we see that the total current through any cross sectionof the tube is
I frac14ethP2
P1
~Js s dlsquo frac14 2
l0
ethU2 U1THORN (15)
which is clearly a constantIf two different tubes of current are bounded by equipoten-
tial lines separated by the same increment U the two tubeshave the same total current Thus in Fig 6 all of the tubeswith Un frac14 01 have the same total current From this ob-servation we see that the current density is largest under thepole of the magnet and smallest near the edge of the disc atangles near u frac14 180 Notice that the tubes of current areclosed and the radial component of the surface current iszero at the edge of the disc The closed tubes of current areanalogous to eddies that form around an object in flowingwater hence the name ldquoeddy currentsrdquo (also ldquoFoucaultcurrentsrdquo) Because of the finite conductivity of the disc theeddy currents dissipate energy This energy must be suppliedby the mechanical source turning the axle of the disc
C Faradayrsquos law and the open-circuit voltage
Faradayrsquos law in integral form isthornCethtTHORN
frac12~Eeth~r tTHORN thorn~veth~r tTHORN ~Beth~r tTHORN d~lsquo frac14 d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S
(16)
where we explicitly indicate that the closed contour Cbounding the open surface S can vary with time and ~v isthe velocity for a point on the contour24 We will apply
Eq (16) to the contour ABCDA in Fig 3(a) shown inmore detail in Fig 7
For this contour in the limit u frac14 xt 0 the expres-sion on the left-hand side of Eq (16) becomes
VethqbubTHORN thornethqb
qfrac140
frac12~Eethqub 0THORN thorn~vethqub 0THORN
~Bethqub 0THORN q dq (17)
The integral in Eq (17) is for the portion of the contourCD that is in the disc where the constitutive equation forthe surface current density in the laboratory frame applieswhich is
~JsethqubTHORN ~Jethqub 0THORNd
frac14 rdfrac12~Eethqub 0THORN thorn~vethqub 0THORN ~Bethqub 0THORN(18)
When Eq (18) is substituted into Eq (17) we obtain
VethqbubTHORN thorn1
rd
ethqb
qfrac140
q ~JsethqubTHORNdq (19)
for our final result for the left-hand side of Eq (16)Now consider the expression on the right-hand-side of Eq
(16) for the contour ABCDA In the time increment t thearea S in Fig 7 increases by the increment S (gray in thefigure) We will assume that the applied magnetic field ismuch greater than axial component of the magnetic field dueto the current in the disc (j~Baj jz ~Bij) and we will ignorethe latter Then the time variation in the flux of the magneticfield through S is due to the applied field ~Ba passingthrough S or
d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S frac14 limt0
1
t
ethqb
qfrac140
~BaethqubTHORN ethzTHORNq u dq
264
375 frac14 lim
t0
ut
ethqb
qfrac140
qBaethqubTHORN dq
264
375 frac14 x
ethqb
qfrac140
qBaethqubTHORN dq
(20)
After equating the left-hand- and right-hand-sides of Eq (16) for the contour ABCDAmdashequating Eqs (19) and (20)mdashweobtain the open-circuit voltage at the terminals A-B in Fig 3(a) to be
Fig 7 Details for contour C used with Faradayrsquos law
911 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 911
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13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
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13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
Faradayrsquos first dynamo A retrospective
Glenn S Smitha)
School of Electrical and Computer Engineering Georgia Institute of Technology AtlantaGeorgia 30332-0250
(Received 28 June 2013 accepted 2 October 2013)
In the early 1830s Michael Faraday performed his seminal experimental research on
electromagnetic induction in which he created the first electric dynamomdasha machine for
continuously converting rotational mechanical energy into electrical energy His machine was a
conducting disc rotating between the poles of a permanent magnet with the voltagecurrent
obtained from brushes contacting the disc In his first dynamo the magnetic field was asymmetric
with respect to the axis of the disc This is to be contrasted with some of his later symmetric
designs which are the ones almost invariably discussed in textbooks on electromagnetism In this
paper a theoretical analysis is developed for Faradayrsquos first dynamo From this analysis the eddy
currents in the disc and the open-circuit voltage for arbitrary positioning of the brushes are
determined The approximate analysis is verified by comparing theoretical results with
measurements made on an experimental recreation of the dynamo Quantitative results from the
analysis are used to elucidate Faradayrsquos qualitative observations from which he learned so much
about electromagnetic induction For the asymmetric design the eddy currents in the disc
dissipate energy that makes the dynamo inefficient prohibiting its use as a practical generator of
electric power Faradayrsquos experiments with his first dynamo provided valuable insight into
electromagnetic induction and this insight was quickly used by others to design practical
generators VC 2013 American Association of Physics Teachers
[httpdxdoiorg10111914825232]
I INTRODUCTION
In 1831 Michael Faraday (Fig 1) embarked on one of themost productive periods of his career during which heexperimented with electromagnetism and among otherthings discovered electromagnetic induction Faraday wasaware of research that had been done earlier on theContinent in particular the experiments on magnetism of theFrench scientist Francois Arago In 1824 Arago discovered aphenomenon that would become known as ldquoAragorsquosrotationsrdquo1 Arago suspended a magnetized needle parallel toand above a copper disc When he rotated the disc about itsaxis he noticed that the needle also rotated in the samedirection as the disc At the time there was much speculationas to the cause of these rotations In his ExperimentalResearches in Electricity Faraday commented that ldquohellipIhope to make the experiment of Arago a new source of elec-tricityhelliprdquo and this he did in his subsequent research2
Faraday invented the first electric dynamosmdashmachines forcontinuously converting rotational mechanical energy intoelectrical energy
Figure 2(a) shows a sketch of Faradayrsquos first dynamo Thissketch is based on a drawing from Faradayrsquos diary datedOctober 28 183134 Probably because of his familiarity withAragorsquos experiment Faraday chose to use a copper discmounted on an axle in his experiment He placed the discbetween the poles of a strong permanent magnet and heused mercury-coated sliding contacts to connect the disc toan external circuit containing a simple but sensitive galva-nometer Faraday called these contacts ldquoelectric collectorsrdquobut we would now call them ldquobrushesrdquo As Faraday rotatedthe disc he observed a continuous deflection of the galva-nometer Faraday performed many experiments with thisdynamo in an effort to understand the physics of electromag-netic induction We will have more to say about these experi-ments later in this paper
After studying his first dynamo Faraday examined otherconfigurations for the dynamo one of which is shown in Fig2(b) This sketch is based on a drawing from SilvanusThompsonrsquos biography of Faraday and the dynamo is dis-cussed in an entry in Faradayrsquos diary dated December 1618315ndash7 Faraday cut a circular hole of slightly bigger
Fig 1 Portrait of Michael Faraday (ca 1840s) taken sometime after the
publication of the first volume of his Experimental Researches inElectricity in which he describes his early dynamos Smithsonian Institution
Archives Image SIA2012-1087
907 Am J Phys 81 (12) December 2013 httpaaptorgajp VC 2013 American Association of Physics Teachers 907
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
diameter than his disc in a lead sheet then he placed the cop-per disc in the hole and filled the space between the disc andsheet with mercury He fastened one lead from his galva-nometer to the sheet and placed the other lead in a mercury-filled cup atop the axle of the disc The magnetic field wasthe Earthrsquos which has a significant component normal to thesurface of the Earth in London hence normal to the horizon-tal disc As Faraday rotated the disc he observed a deflectionof the galvanometer Notice that unlike Faradayrsquos firstdynamo all of the components of this dynamo (the disc thebrush formed by the mercury-filled trough and the compo-nent of the magnetic field normal to the disc) are rotationallysymmetric about the axis of the disc
Most textbooks on electromagnetism contain a discussion orproblem involving a symmetrical dynamo which in almost allrespects is the same as Faradayrsquos design in Fig 2(b) Sometimesit is referred to as a ldquounipolar generatorrdquo or a ldquohomopolar gener-atorrdquo Because of the simplicity of the symmetrical structure asolution for the open-circuit voltage V at the terminals A-B iseasily found by a few different methods to be
V frac14 xB0A2
2 (1)
where A and x are the radius and the angular frequency forthe disc and B0 is the component of the applied magneticfield that is normal to the disc Experimental results that ver-ify Eq (1) have been presented in a number of papers8ndash12
and more detailed discussions of the symmetrical dynamoare in the books of Woodson and Melcher and Van Bladeland in the papers of Van Bladel and Montgomery13ndash16
Faradayrsquos first dynamo the asymmetric one shown in Fig2(a) has received much less attention There is no mentionof it in most textbooks on electromagnetism In a paper from1942 and later in the third edition of his graduate-level text-book William Smythe analyzed a geometry similar toFaradayrsquos but he did not discuss it in the context of adynamo for example he did not determine the open-circuitvoltage1718
The purpose of this paper is to present a detailed discussionof Faradayrsquos first dynamo supported by new analytical and ex-perimental results This material particularly the graphicscan be used to present the historically important story ofFaradayrsquos accomplishments to students in undergraduate andgraduate courses in electromagnetism In Sec II we describean analysis of the dynamo in which Smythersquos approximateresult for the magnetic scalar potential is used to obtain thecurrent in the disc and we extend this result to include theopen-circuit voltage for all points on the disc In Sec III wepresent quantitative numerical results from the analysis andshow how these results are related to Faradayrsquos qualitativeobservations In Sec IV we describe an experiment that issimilar to Faradayrsquos but based on modern materials and instru-mentation Measurements from this experiment validate theapproximate analysis Finally Sec V contains a discussion inwhich we address the question ldquoWhat ever became ofFaradayrsquos first dynamordquo or stated differently ldquoHow is hismachine used todayrdquo
II ANALYSIS OF FARADAYrsquoS FIRST DYNAMO
The analysis for the dynamo is based on the model shownin Fig 3(a) the coordinates and dimensions are on the planview of the disc in Fig 3(b) The circular disc of radius Aand thickness d has electrical conductivity r permeabilityl0 and rotates with angular frequency x The applied axialmagnetic field ~Ba frac14 B0z is uniform over the circular area ofradius a located at a distance c from the axis of the disc(gray area in the figure) The external circuit formed fromperfectly conducting wire makes contact with the disc at thebrush on the axis (C) and at the brush at the point ethqbubTHORN onthe disc (D) The open-circuit voltage V is determined at theterminals A-B in the external circuit The analysis is per-formed in the laboratory frame which is the frame in whichthe magnet and the external circuit are at rest The electro-magnetic field is time-invariant in this frame because of therotational symmetry of the disc To see this consider whathappens when a hole is cut into the disc destroying the rota-tional symmetry The electromagnetic field in the laboratoryframe is then a periodic function of time
The analysis is a quasi-static one in which magneticeffects are assumed to be dominant and all dimensions areelectrically small so that any retardation in time for the fieldcan be ignored19 In Maxwellrsquos equations the displacementcurrent ~D=t and the volume charge density q are ignoredThe latter condition means that any convection current dueto the motion of free charge is also ignored In addition tothe applied magnetic field ~Ba there is the magnetic field ~Bi
Fig 2 (a) Faradayrsquos first dynamo based on a drawing from Faradayrsquos di-
ary3 (b) One of Faradayrsquos rotationally symmetric configurations for a
dynamo based on a drawing by Thompson5
908 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 908
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
due to the current induced in the disc In the source-freeregion outside the disc the two Maxwellrsquos equations thatinvolve the magnetic field ~Bi are
r ~Bi frac14 0 (2)
and
r ~Bi 0 (3)
The volume density for the conduction current ~J is assumedto be uniform throughout the thickness of the disc with anegligible axial component Thus it can be approximated bya surface- or sheet-current density ~Js ~Jd20
The boundary condition that relates the surface currentdensity to the magnetic field is
~JsethquTHORN frac141
l0
z frac12~Biethqu z frac14 0thornTHORN ~Biethqu z frac14 0THORN
frac14 2
l0
z ~Biethqu z frac14 0thornTHORN (4)
where for the last term we have used the fact that the compo-nent of the magnetic field tangential to the surface of the dischas odd symmetry about the disc as shown in Fig 4(a)
A Magnetic scalar potential
We can represent the irrotational magnetic field Bi by ascalar magnetic potential U via21
~Bi frac14 rU (5)
This is inserted into Eq (2) to obtain Laplacersquos equation forthe potential in a source-free region
r2U frac14 0 (6)
For describing the potential at the top surface of the disc(zfrac14 0thorn) we will define the three regions on the disc shownin Fig 5 The two radial lines at ua frac14 6sin1etha=cTHORN are tan-gent to the boundary of the circular region containing theapplied magnetic field Region I (light gray) is bounded bythese lines (ua u ua) and is above the applied mag-netic field qo lt q A with qo frac14 cfrac12cosu
thornffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region II (dark gray) is within the
applied magnetic field ua u ua and qi q qo
with qi frac14 cfrac12cosuffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region III (white) is
everywhere else on the disc Using this notation the appliedmagnetic field can be expressed as
~BaethquTHORN frac14 BaethquTHORNzfrac14 B0fUfrac12q qiethuTHORN Ufrac12q qoethuTHORNgfrac12Uethuthorn uaTHORN Uethu uaTHORNz (7)
in which U(n) is the Heaviside unit-step function
Fig 3 (a) Model used in the analysis of the dynamo (b) Plan view of the
disc showing the coordinates and dimensions
Fig 4 Details for the surface current in the disc (a) Boundary condition
relating the magnetic field to the surface current density (b) Tube of surface
current showing coordinates
909 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 909
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
Smythe gives approximate expressions for the magnetic scalar potential in these regions as171822
UIethqnu z frac14 0thornTHORN frac14 UIIIethqnu z frac14 0thornTHORN frac14 xB0Acrd
2a2
nqnsinu1
q2n thorn c2
n 2cnqncosu 1
c2nq
2n thorn 1 2cnqncosu
(8)
and
UIIethqnu z frac14 0thornTHORN
frac14 xB0Acrd
2qnsinu 1 a2
n
c2nq
2n thorn 1 2cnqncosu
(9)
in which we have normalized the dimensions to the radius ofthe disc that is qn frac14 q=A an frac14 a=A etc
Figure 6 is a contour plot of the scalar potential normal-ized so that maxjUnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 These parameters are roughly the same as thoseused for the experiments described later All of the contoursare spaced by the increment Un frac14 01 except the incom-plete contours for Un frac14 6001 and 6 005 Notice that thepotential has odd symmetry about the line u frac14 0 180
(positive on the left and negative on the right) and the poten-tial is zero along that line and along the edge of the discwhere qfrac14A
B Surface current density
We are generally more used to interpreting the surfacecurrent density than the magnetic scalar potential and theformer is easily obtained from the latter Inserting Eq (5)into Eq (4) we obtain
~JsethquTHORN frac14 2
l0
z r2Uethqu z frac14 0thornTHORN (10)
where we have use r2 to indicate that the gradient is onlywith respect to the two variables q u
The equipotential lines (Ufrac14 constant) such as those inFig 6 are also streamlines of the surface current densitythat is at every point along one of these lines the surface cur-rent is tangential to the line To show this we first note thatr2U is normal to the equipotential lines The operation
r2U ~Js frac14 2
lo
r2U ethz r2UTHORN
frac14 2
lo
z ethr2Ur2UTHORN frac14 0 (11)
shows that the surface current density is normal to r2UHence the surface current is parallel or tangential to theequipotential lines
Two adjacent equipotential lines such as the lines for U1
and U2 in Fig 4(b) bound a two-dimensional tube of surfacecurrent23 At any cross section of the tube the total current Ithrough the tube is the same To show this we first recallfrom Eq (3) that the magnetic field is irrotational so in anyregion in which the field is well defined the line integral of~Bi between two points such as from P1 to P2 in Fig 4(b) isindependent of the path of integration21 Thus
ethP2
P1
~Bi t dlsquo frac14 ethP2
P1
r2U t dlsquo frac14 ethU2 U1THORN (12)
Fig 5 Regions and coordinates used in the description of the scalar mag-
netic potential U at the top surface (zfrac14 0thorn) of the disc
Fig 6 Contour plot for the magnetic scalar potential Unethqu z frac14 0thornTHORN for
the case aAfrac14 0170 and cAfrac14 0667 The potential is normalized so that
maxjUnj frac14 10 and the contours are spaced by the increment Un frac14 01
except the incomplete contours for Unfrac146001 and 6005 The equipoten-
tial lines are also streamlines of the surface current density and the arrows
on these lines show the direction of the current Two adjacent equipotential
lines bound a tube of surface current through which the total current I is the
same at any cross section
910 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 910
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13023920174 On Sun 24 Aug 2014 212302
where t is a unit vector tangent to the path After taking frac12zEq (4) t and rearranging terms we obtain
~Bi t frac14 l0
2ethz ~JsTHORN t (13)
Substituting Eq (13) into the left-hand side of Eq (12) gives
l0
2
ethP2
P1
ethz ~JsTHORN t dlsquo frac14 l0
2
ethP2
P1
~Js s dlsquo frac14 ethU2 U1THORN
(14)
in which the unit vector s frac14 z t is in the plane of the discand normal to the path as shown in Fig 4(b) Now from Eq(14) we see that the total current through any cross sectionof the tube is
I frac14ethP2
P1
~Js s dlsquo frac14 2
l0
ethU2 U1THORN (15)
which is clearly a constantIf two different tubes of current are bounded by equipoten-
tial lines separated by the same increment U the two tubeshave the same total current Thus in Fig 6 all of the tubeswith Un frac14 01 have the same total current From this ob-servation we see that the current density is largest under thepole of the magnet and smallest near the edge of the disc atangles near u frac14 180 Notice that the tubes of current areclosed and the radial component of the surface current iszero at the edge of the disc The closed tubes of current areanalogous to eddies that form around an object in flowingwater hence the name ldquoeddy currentsrdquo (also ldquoFoucaultcurrentsrdquo) Because of the finite conductivity of the disc theeddy currents dissipate energy This energy must be suppliedby the mechanical source turning the axle of the disc
C Faradayrsquos law and the open-circuit voltage
Faradayrsquos law in integral form isthornCethtTHORN
frac12~Eeth~r tTHORN thorn~veth~r tTHORN ~Beth~r tTHORN d~lsquo frac14 d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S
(16)
where we explicitly indicate that the closed contour Cbounding the open surface S can vary with time and ~v isthe velocity for a point on the contour24 We will apply
Eq (16) to the contour ABCDA in Fig 3(a) shown inmore detail in Fig 7
For this contour in the limit u frac14 xt 0 the expres-sion on the left-hand side of Eq (16) becomes
VethqbubTHORN thornethqb
qfrac140
frac12~Eethqub 0THORN thorn~vethqub 0THORN
~Bethqub 0THORN q dq (17)
The integral in Eq (17) is for the portion of the contourCD that is in the disc where the constitutive equation forthe surface current density in the laboratory frame applieswhich is
~JsethqubTHORN ~Jethqub 0THORNd
frac14 rdfrac12~Eethqub 0THORN thorn~vethqub 0THORN ~Bethqub 0THORN(18)
When Eq (18) is substituted into Eq (17) we obtain
VethqbubTHORN thorn1
rd
ethqb
qfrac140
q ~JsethqubTHORNdq (19)
for our final result for the left-hand side of Eq (16)Now consider the expression on the right-hand-side of Eq
(16) for the contour ABCDA In the time increment t thearea S in Fig 7 increases by the increment S (gray in thefigure) We will assume that the applied magnetic field ismuch greater than axial component of the magnetic field dueto the current in the disc (j~Baj jz ~Bij) and we will ignorethe latter Then the time variation in the flux of the magneticfield through S is due to the applied field ~Ba passingthrough S or
d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S frac14 limt0
1
t
ethqb
qfrac140
~BaethqubTHORN ethzTHORNq u dq
264
375 frac14 lim
t0
ut
ethqb
qfrac140
qBaethqubTHORN dq
264
375 frac14 x
ethqb
qfrac140
qBaethqubTHORN dq
(20)
After equating the left-hand- and right-hand-sides of Eq (16) for the contour ABCDAmdashequating Eqs (19) and (20)mdashweobtain the open-circuit voltage at the terminals A-B in Fig 3(a) to be
Fig 7 Details for contour C used with Faradayrsquos law
911 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 911
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13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
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13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
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13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
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13023920174 On Sun 24 Aug 2014 212302
diameter than his disc in a lead sheet then he placed the cop-per disc in the hole and filled the space between the disc andsheet with mercury He fastened one lead from his galva-nometer to the sheet and placed the other lead in a mercury-filled cup atop the axle of the disc The magnetic field wasthe Earthrsquos which has a significant component normal to thesurface of the Earth in London hence normal to the horizon-tal disc As Faraday rotated the disc he observed a deflectionof the galvanometer Notice that unlike Faradayrsquos firstdynamo all of the components of this dynamo (the disc thebrush formed by the mercury-filled trough and the compo-nent of the magnetic field normal to the disc) are rotationallysymmetric about the axis of the disc
Most textbooks on electromagnetism contain a discussion orproblem involving a symmetrical dynamo which in almost allrespects is the same as Faradayrsquos design in Fig 2(b) Sometimesit is referred to as a ldquounipolar generatorrdquo or a ldquohomopolar gener-atorrdquo Because of the simplicity of the symmetrical structure asolution for the open-circuit voltage V at the terminals A-B iseasily found by a few different methods to be
V frac14 xB0A2
2 (1)
where A and x are the radius and the angular frequency forthe disc and B0 is the component of the applied magneticfield that is normal to the disc Experimental results that ver-ify Eq (1) have been presented in a number of papers8ndash12
and more detailed discussions of the symmetrical dynamoare in the books of Woodson and Melcher and Van Bladeland in the papers of Van Bladel and Montgomery13ndash16
Faradayrsquos first dynamo the asymmetric one shown in Fig2(a) has received much less attention There is no mentionof it in most textbooks on electromagnetism In a paper from1942 and later in the third edition of his graduate-level text-book William Smythe analyzed a geometry similar toFaradayrsquos but he did not discuss it in the context of adynamo for example he did not determine the open-circuitvoltage1718
The purpose of this paper is to present a detailed discussionof Faradayrsquos first dynamo supported by new analytical and ex-perimental results This material particularly the graphicscan be used to present the historically important story ofFaradayrsquos accomplishments to students in undergraduate andgraduate courses in electromagnetism In Sec II we describean analysis of the dynamo in which Smythersquos approximateresult for the magnetic scalar potential is used to obtain thecurrent in the disc and we extend this result to include theopen-circuit voltage for all points on the disc In Sec III wepresent quantitative numerical results from the analysis andshow how these results are related to Faradayrsquos qualitativeobservations In Sec IV we describe an experiment that issimilar to Faradayrsquos but based on modern materials and instru-mentation Measurements from this experiment validate theapproximate analysis Finally Sec V contains a discussion inwhich we address the question ldquoWhat ever became ofFaradayrsquos first dynamordquo or stated differently ldquoHow is hismachine used todayrdquo
II ANALYSIS OF FARADAYrsquoS FIRST DYNAMO
The analysis for the dynamo is based on the model shownin Fig 3(a) the coordinates and dimensions are on the planview of the disc in Fig 3(b) The circular disc of radius Aand thickness d has electrical conductivity r permeabilityl0 and rotates with angular frequency x The applied axialmagnetic field ~Ba frac14 B0z is uniform over the circular area ofradius a located at a distance c from the axis of the disc(gray area in the figure) The external circuit formed fromperfectly conducting wire makes contact with the disc at thebrush on the axis (C) and at the brush at the point ethqbubTHORN onthe disc (D) The open-circuit voltage V is determined at theterminals A-B in the external circuit The analysis is per-formed in the laboratory frame which is the frame in whichthe magnet and the external circuit are at rest The electro-magnetic field is time-invariant in this frame because of therotational symmetry of the disc To see this consider whathappens when a hole is cut into the disc destroying the rota-tional symmetry The electromagnetic field in the laboratoryframe is then a periodic function of time
The analysis is a quasi-static one in which magneticeffects are assumed to be dominant and all dimensions areelectrically small so that any retardation in time for the fieldcan be ignored19 In Maxwellrsquos equations the displacementcurrent ~D=t and the volume charge density q are ignoredThe latter condition means that any convection current dueto the motion of free charge is also ignored In addition tothe applied magnetic field ~Ba there is the magnetic field ~Bi
Fig 2 (a) Faradayrsquos first dynamo based on a drawing from Faradayrsquos di-
ary3 (b) One of Faradayrsquos rotationally symmetric configurations for a
dynamo based on a drawing by Thompson5
908 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 908
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13023920174 On Sun 24 Aug 2014 212302
due to the current induced in the disc In the source-freeregion outside the disc the two Maxwellrsquos equations thatinvolve the magnetic field ~Bi are
r ~Bi frac14 0 (2)
and
r ~Bi 0 (3)
The volume density for the conduction current ~J is assumedto be uniform throughout the thickness of the disc with anegligible axial component Thus it can be approximated bya surface- or sheet-current density ~Js ~Jd20
The boundary condition that relates the surface currentdensity to the magnetic field is
~JsethquTHORN frac141
l0
z frac12~Biethqu z frac14 0thornTHORN ~Biethqu z frac14 0THORN
frac14 2
l0
z ~Biethqu z frac14 0thornTHORN (4)
where for the last term we have used the fact that the compo-nent of the magnetic field tangential to the surface of the dischas odd symmetry about the disc as shown in Fig 4(a)
A Magnetic scalar potential
We can represent the irrotational magnetic field Bi by ascalar magnetic potential U via21
~Bi frac14 rU (5)
This is inserted into Eq (2) to obtain Laplacersquos equation forthe potential in a source-free region
r2U frac14 0 (6)
For describing the potential at the top surface of the disc(zfrac14 0thorn) we will define the three regions on the disc shownin Fig 5 The two radial lines at ua frac14 6sin1etha=cTHORN are tan-gent to the boundary of the circular region containing theapplied magnetic field Region I (light gray) is bounded bythese lines (ua u ua) and is above the applied mag-netic field qo lt q A with qo frac14 cfrac12cosu
thornffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region II (dark gray) is within the
applied magnetic field ua u ua and qi q qo
with qi frac14 cfrac12cosuffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region III (white) is
everywhere else on the disc Using this notation the appliedmagnetic field can be expressed as
~BaethquTHORN frac14 BaethquTHORNzfrac14 B0fUfrac12q qiethuTHORN Ufrac12q qoethuTHORNgfrac12Uethuthorn uaTHORN Uethu uaTHORNz (7)
in which U(n) is the Heaviside unit-step function
Fig 3 (a) Model used in the analysis of the dynamo (b) Plan view of the
disc showing the coordinates and dimensions
Fig 4 Details for the surface current in the disc (a) Boundary condition
relating the magnetic field to the surface current density (b) Tube of surface
current showing coordinates
909 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 909
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13023920174 On Sun 24 Aug 2014 212302
Smythe gives approximate expressions for the magnetic scalar potential in these regions as171822
UIethqnu z frac14 0thornTHORN frac14 UIIIethqnu z frac14 0thornTHORN frac14 xB0Acrd
2a2
nqnsinu1
q2n thorn c2
n 2cnqncosu 1
c2nq
2n thorn 1 2cnqncosu
(8)
and
UIIethqnu z frac14 0thornTHORN
frac14 xB0Acrd
2qnsinu 1 a2
n
c2nq
2n thorn 1 2cnqncosu
(9)
in which we have normalized the dimensions to the radius ofthe disc that is qn frac14 q=A an frac14 a=A etc
Figure 6 is a contour plot of the scalar potential normal-ized so that maxjUnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 These parameters are roughly the same as thoseused for the experiments described later All of the contoursare spaced by the increment Un frac14 01 except the incom-plete contours for Un frac14 6001 and 6 005 Notice that thepotential has odd symmetry about the line u frac14 0 180
(positive on the left and negative on the right) and the poten-tial is zero along that line and along the edge of the discwhere qfrac14A
B Surface current density
We are generally more used to interpreting the surfacecurrent density than the magnetic scalar potential and theformer is easily obtained from the latter Inserting Eq (5)into Eq (4) we obtain
~JsethquTHORN frac14 2
l0
z r2Uethqu z frac14 0thornTHORN (10)
where we have use r2 to indicate that the gradient is onlywith respect to the two variables q u
The equipotential lines (Ufrac14 constant) such as those inFig 6 are also streamlines of the surface current densitythat is at every point along one of these lines the surface cur-rent is tangential to the line To show this we first note thatr2U is normal to the equipotential lines The operation
r2U ~Js frac14 2
lo
r2U ethz r2UTHORN
frac14 2
lo
z ethr2Ur2UTHORN frac14 0 (11)
shows that the surface current density is normal to r2UHence the surface current is parallel or tangential to theequipotential lines
Two adjacent equipotential lines such as the lines for U1
and U2 in Fig 4(b) bound a two-dimensional tube of surfacecurrent23 At any cross section of the tube the total current Ithrough the tube is the same To show this we first recallfrom Eq (3) that the magnetic field is irrotational so in anyregion in which the field is well defined the line integral of~Bi between two points such as from P1 to P2 in Fig 4(b) isindependent of the path of integration21 Thus
ethP2
P1
~Bi t dlsquo frac14 ethP2
P1
r2U t dlsquo frac14 ethU2 U1THORN (12)
Fig 5 Regions and coordinates used in the description of the scalar mag-
netic potential U at the top surface (zfrac14 0thorn) of the disc
Fig 6 Contour plot for the magnetic scalar potential Unethqu z frac14 0thornTHORN for
the case aAfrac14 0170 and cAfrac14 0667 The potential is normalized so that
maxjUnj frac14 10 and the contours are spaced by the increment Un frac14 01
except the incomplete contours for Unfrac146001 and 6005 The equipoten-
tial lines are also streamlines of the surface current density and the arrows
on these lines show the direction of the current Two adjacent equipotential
lines bound a tube of surface current through which the total current I is the
same at any cross section
910 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 910
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13023920174 On Sun 24 Aug 2014 212302
where t is a unit vector tangent to the path After taking frac12zEq (4) t and rearranging terms we obtain
~Bi t frac14 l0
2ethz ~JsTHORN t (13)
Substituting Eq (13) into the left-hand side of Eq (12) gives
l0
2
ethP2
P1
ethz ~JsTHORN t dlsquo frac14 l0
2
ethP2
P1
~Js s dlsquo frac14 ethU2 U1THORN
(14)
in which the unit vector s frac14 z t is in the plane of the discand normal to the path as shown in Fig 4(b) Now from Eq(14) we see that the total current through any cross sectionof the tube is
I frac14ethP2
P1
~Js s dlsquo frac14 2
l0
ethU2 U1THORN (15)
which is clearly a constantIf two different tubes of current are bounded by equipoten-
tial lines separated by the same increment U the two tubeshave the same total current Thus in Fig 6 all of the tubeswith Un frac14 01 have the same total current From this ob-servation we see that the current density is largest under thepole of the magnet and smallest near the edge of the disc atangles near u frac14 180 Notice that the tubes of current areclosed and the radial component of the surface current iszero at the edge of the disc The closed tubes of current areanalogous to eddies that form around an object in flowingwater hence the name ldquoeddy currentsrdquo (also ldquoFoucaultcurrentsrdquo) Because of the finite conductivity of the disc theeddy currents dissipate energy This energy must be suppliedby the mechanical source turning the axle of the disc
C Faradayrsquos law and the open-circuit voltage
Faradayrsquos law in integral form isthornCethtTHORN
frac12~Eeth~r tTHORN thorn~veth~r tTHORN ~Beth~r tTHORN d~lsquo frac14 d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S
(16)
where we explicitly indicate that the closed contour Cbounding the open surface S can vary with time and ~v isthe velocity for a point on the contour24 We will apply
Eq (16) to the contour ABCDA in Fig 3(a) shown inmore detail in Fig 7
For this contour in the limit u frac14 xt 0 the expres-sion on the left-hand side of Eq (16) becomes
VethqbubTHORN thornethqb
qfrac140
frac12~Eethqub 0THORN thorn~vethqub 0THORN
~Bethqub 0THORN q dq (17)
The integral in Eq (17) is for the portion of the contourCD that is in the disc where the constitutive equation forthe surface current density in the laboratory frame applieswhich is
~JsethqubTHORN ~Jethqub 0THORNd
frac14 rdfrac12~Eethqub 0THORN thorn~vethqub 0THORN ~Bethqub 0THORN(18)
When Eq (18) is substituted into Eq (17) we obtain
VethqbubTHORN thorn1
rd
ethqb
qfrac140
q ~JsethqubTHORNdq (19)
for our final result for the left-hand side of Eq (16)Now consider the expression on the right-hand-side of Eq
(16) for the contour ABCDA In the time increment t thearea S in Fig 7 increases by the increment S (gray in thefigure) We will assume that the applied magnetic field ismuch greater than axial component of the magnetic field dueto the current in the disc (j~Baj jz ~Bij) and we will ignorethe latter Then the time variation in the flux of the magneticfield through S is due to the applied field ~Ba passingthrough S or
d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S frac14 limt0
1
t
ethqb
qfrac140
~BaethqubTHORN ethzTHORNq u dq
264
375 frac14 lim
t0
ut
ethqb
qfrac140
qBaethqubTHORN dq
264
375 frac14 x
ethqb
qfrac140
qBaethqubTHORN dq
(20)
After equating the left-hand- and right-hand-sides of Eq (16) for the contour ABCDAmdashequating Eqs (19) and (20)mdashweobtain the open-circuit voltage at the terminals A-B in Fig 3(a) to be
Fig 7 Details for contour C used with Faradayrsquos law
911 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 911
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13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
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13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
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13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
due to the current induced in the disc In the source-freeregion outside the disc the two Maxwellrsquos equations thatinvolve the magnetic field ~Bi are
r ~Bi frac14 0 (2)
and
r ~Bi 0 (3)
The volume density for the conduction current ~J is assumedto be uniform throughout the thickness of the disc with anegligible axial component Thus it can be approximated bya surface- or sheet-current density ~Js ~Jd20
The boundary condition that relates the surface currentdensity to the magnetic field is
~JsethquTHORN frac141
l0
z frac12~Biethqu z frac14 0thornTHORN ~Biethqu z frac14 0THORN
frac14 2
l0
z ~Biethqu z frac14 0thornTHORN (4)
where for the last term we have used the fact that the compo-nent of the magnetic field tangential to the surface of the dischas odd symmetry about the disc as shown in Fig 4(a)
A Magnetic scalar potential
We can represent the irrotational magnetic field Bi by ascalar magnetic potential U via21
~Bi frac14 rU (5)
This is inserted into Eq (2) to obtain Laplacersquos equation forthe potential in a source-free region
r2U frac14 0 (6)
For describing the potential at the top surface of the disc(zfrac14 0thorn) we will define the three regions on the disc shownin Fig 5 The two radial lines at ua frac14 6sin1etha=cTHORN are tan-gent to the boundary of the circular region containing theapplied magnetic field Region I (light gray) is bounded bythese lines (ua u ua) and is above the applied mag-netic field qo lt q A with qo frac14 cfrac12cosu
thornffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region II (dark gray) is within the
applied magnetic field ua u ua and qi q qo
with qi frac14 cfrac12cosuffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffietha=cTHORN2 sin2u
q Region III (white) is
everywhere else on the disc Using this notation the appliedmagnetic field can be expressed as
~BaethquTHORN frac14 BaethquTHORNzfrac14 B0fUfrac12q qiethuTHORN Ufrac12q qoethuTHORNgfrac12Uethuthorn uaTHORN Uethu uaTHORNz (7)
in which U(n) is the Heaviside unit-step function
Fig 3 (a) Model used in the analysis of the dynamo (b) Plan view of the
disc showing the coordinates and dimensions
Fig 4 Details for the surface current in the disc (a) Boundary condition
relating the magnetic field to the surface current density (b) Tube of surface
current showing coordinates
909 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 909
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
Smythe gives approximate expressions for the magnetic scalar potential in these regions as171822
UIethqnu z frac14 0thornTHORN frac14 UIIIethqnu z frac14 0thornTHORN frac14 xB0Acrd
2a2
nqnsinu1
q2n thorn c2
n 2cnqncosu 1
c2nq
2n thorn 1 2cnqncosu
(8)
and
UIIethqnu z frac14 0thornTHORN
frac14 xB0Acrd
2qnsinu 1 a2
n
c2nq
2n thorn 1 2cnqncosu
(9)
in which we have normalized the dimensions to the radius ofthe disc that is qn frac14 q=A an frac14 a=A etc
Figure 6 is a contour plot of the scalar potential normal-ized so that maxjUnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 These parameters are roughly the same as thoseused for the experiments described later All of the contoursare spaced by the increment Un frac14 01 except the incom-plete contours for Un frac14 6001 and 6 005 Notice that thepotential has odd symmetry about the line u frac14 0 180
(positive on the left and negative on the right) and the poten-tial is zero along that line and along the edge of the discwhere qfrac14A
B Surface current density
We are generally more used to interpreting the surfacecurrent density than the magnetic scalar potential and theformer is easily obtained from the latter Inserting Eq (5)into Eq (4) we obtain
~JsethquTHORN frac14 2
l0
z r2Uethqu z frac14 0thornTHORN (10)
where we have use r2 to indicate that the gradient is onlywith respect to the two variables q u
The equipotential lines (Ufrac14 constant) such as those inFig 6 are also streamlines of the surface current densitythat is at every point along one of these lines the surface cur-rent is tangential to the line To show this we first note thatr2U is normal to the equipotential lines The operation
r2U ~Js frac14 2
lo
r2U ethz r2UTHORN
frac14 2
lo
z ethr2Ur2UTHORN frac14 0 (11)
shows that the surface current density is normal to r2UHence the surface current is parallel or tangential to theequipotential lines
Two adjacent equipotential lines such as the lines for U1
and U2 in Fig 4(b) bound a two-dimensional tube of surfacecurrent23 At any cross section of the tube the total current Ithrough the tube is the same To show this we first recallfrom Eq (3) that the magnetic field is irrotational so in anyregion in which the field is well defined the line integral of~Bi between two points such as from P1 to P2 in Fig 4(b) isindependent of the path of integration21 Thus
ethP2
P1
~Bi t dlsquo frac14 ethP2
P1
r2U t dlsquo frac14 ethU2 U1THORN (12)
Fig 5 Regions and coordinates used in the description of the scalar mag-
netic potential U at the top surface (zfrac14 0thorn) of the disc
Fig 6 Contour plot for the magnetic scalar potential Unethqu z frac14 0thornTHORN for
the case aAfrac14 0170 and cAfrac14 0667 The potential is normalized so that
maxjUnj frac14 10 and the contours are spaced by the increment Un frac14 01
except the incomplete contours for Unfrac146001 and 6005 The equipoten-
tial lines are also streamlines of the surface current density and the arrows
on these lines show the direction of the current Two adjacent equipotential
lines bound a tube of surface current through which the total current I is the
same at any cross section
910 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 910
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
where t is a unit vector tangent to the path After taking frac12zEq (4) t and rearranging terms we obtain
~Bi t frac14 l0
2ethz ~JsTHORN t (13)
Substituting Eq (13) into the left-hand side of Eq (12) gives
l0
2
ethP2
P1
ethz ~JsTHORN t dlsquo frac14 l0
2
ethP2
P1
~Js s dlsquo frac14 ethU2 U1THORN
(14)
in which the unit vector s frac14 z t is in the plane of the discand normal to the path as shown in Fig 4(b) Now from Eq(14) we see that the total current through any cross sectionof the tube is
I frac14ethP2
P1
~Js s dlsquo frac14 2
l0
ethU2 U1THORN (15)
which is clearly a constantIf two different tubes of current are bounded by equipoten-
tial lines separated by the same increment U the two tubeshave the same total current Thus in Fig 6 all of the tubeswith Un frac14 01 have the same total current From this ob-servation we see that the current density is largest under thepole of the magnet and smallest near the edge of the disc atangles near u frac14 180 Notice that the tubes of current areclosed and the radial component of the surface current iszero at the edge of the disc The closed tubes of current areanalogous to eddies that form around an object in flowingwater hence the name ldquoeddy currentsrdquo (also ldquoFoucaultcurrentsrdquo) Because of the finite conductivity of the disc theeddy currents dissipate energy This energy must be suppliedby the mechanical source turning the axle of the disc
C Faradayrsquos law and the open-circuit voltage
Faradayrsquos law in integral form isthornCethtTHORN
frac12~Eeth~r tTHORN thorn~veth~r tTHORN ~Beth~r tTHORN d~lsquo frac14 d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S
(16)
where we explicitly indicate that the closed contour Cbounding the open surface S can vary with time and ~v isthe velocity for a point on the contour24 We will apply
Eq (16) to the contour ABCDA in Fig 3(a) shown inmore detail in Fig 7
For this contour in the limit u frac14 xt 0 the expres-sion on the left-hand side of Eq (16) becomes
VethqbubTHORN thornethqb
qfrac140
frac12~Eethqub 0THORN thorn~vethqub 0THORN
~Bethqub 0THORN q dq (17)
The integral in Eq (17) is for the portion of the contourCD that is in the disc where the constitutive equation forthe surface current density in the laboratory frame applieswhich is
~JsethqubTHORN ~Jethqub 0THORNd
frac14 rdfrac12~Eethqub 0THORN thorn~vethqub 0THORN ~Bethqub 0THORN(18)
When Eq (18) is substituted into Eq (17) we obtain
VethqbubTHORN thorn1
rd
ethqb
qfrac140
q ~JsethqubTHORNdq (19)
for our final result for the left-hand side of Eq (16)Now consider the expression on the right-hand-side of Eq
(16) for the contour ABCDA In the time increment t thearea S in Fig 7 increases by the increment S (gray in thefigure) We will assume that the applied magnetic field ismuch greater than axial component of the magnetic field dueto the current in the disc (j~Baj jz ~Bij) and we will ignorethe latter Then the time variation in the flux of the magneticfield through S is due to the applied field ~Ba passingthrough S or
d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S frac14 limt0
1
t
ethqb
qfrac140
~BaethqubTHORN ethzTHORNq u dq
264
375 frac14 lim
t0
ut
ethqb
qfrac140
qBaethqubTHORN dq
264
375 frac14 x
ethqb
qfrac140
qBaethqubTHORN dq
(20)
After equating the left-hand- and right-hand-sides of Eq (16) for the contour ABCDAmdashequating Eqs (19) and (20)mdashweobtain the open-circuit voltage at the terminals A-B in Fig 3(a) to be
Fig 7 Details for contour C used with Faradayrsquos law
911 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 911
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
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13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
Smythe gives approximate expressions for the magnetic scalar potential in these regions as171822
UIethqnu z frac14 0thornTHORN frac14 UIIIethqnu z frac14 0thornTHORN frac14 xB0Acrd
2a2
nqnsinu1
q2n thorn c2
n 2cnqncosu 1
c2nq
2n thorn 1 2cnqncosu
(8)
and
UIIethqnu z frac14 0thornTHORN
frac14 xB0Acrd
2qnsinu 1 a2
n
c2nq
2n thorn 1 2cnqncosu
(9)
in which we have normalized the dimensions to the radius ofthe disc that is qn frac14 q=A an frac14 a=A etc
Figure 6 is a contour plot of the scalar potential normal-ized so that maxjUnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 These parameters are roughly the same as thoseused for the experiments described later All of the contoursare spaced by the increment Un frac14 01 except the incom-plete contours for Un frac14 6001 and 6 005 Notice that thepotential has odd symmetry about the line u frac14 0 180
(positive on the left and negative on the right) and the poten-tial is zero along that line and along the edge of the discwhere qfrac14A
B Surface current density
We are generally more used to interpreting the surfacecurrent density than the magnetic scalar potential and theformer is easily obtained from the latter Inserting Eq (5)into Eq (4) we obtain
~JsethquTHORN frac14 2
l0
z r2Uethqu z frac14 0thornTHORN (10)
where we have use r2 to indicate that the gradient is onlywith respect to the two variables q u
The equipotential lines (Ufrac14 constant) such as those inFig 6 are also streamlines of the surface current densitythat is at every point along one of these lines the surface cur-rent is tangential to the line To show this we first note thatr2U is normal to the equipotential lines The operation
r2U ~Js frac14 2
lo
r2U ethz r2UTHORN
frac14 2
lo
z ethr2Ur2UTHORN frac14 0 (11)
shows that the surface current density is normal to r2UHence the surface current is parallel or tangential to theequipotential lines
Two adjacent equipotential lines such as the lines for U1
and U2 in Fig 4(b) bound a two-dimensional tube of surfacecurrent23 At any cross section of the tube the total current Ithrough the tube is the same To show this we first recallfrom Eq (3) that the magnetic field is irrotational so in anyregion in which the field is well defined the line integral of~Bi between two points such as from P1 to P2 in Fig 4(b) isindependent of the path of integration21 Thus
ethP2
P1
~Bi t dlsquo frac14 ethP2
P1
r2U t dlsquo frac14 ethU2 U1THORN (12)
Fig 5 Regions and coordinates used in the description of the scalar mag-
netic potential U at the top surface (zfrac14 0thorn) of the disc
Fig 6 Contour plot for the magnetic scalar potential Unethqu z frac14 0thornTHORN for
the case aAfrac14 0170 and cAfrac14 0667 The potential is normalized so that
maxjUnj frac14 10 and the contours are spaced by the increment Un frac14 01
except the incomplete contours for Unfrac146001 and 6005 The equipoten-
tial lines are also streamlines of the surface current density and the arrows
on these lines show the direction of the current Two adjacent equipotential
lines bound a tube of surface current through which the total current I is the
same at any cross section
910 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 910
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
where t is a unit vector tangent to the path After taking frac12zEq (4) t and rearranging terms we obtain
~Bi t frac14 l0
2ethz ~JsTHORN t (13)
Substituting Eq (13) into the left-hand side of Eq (12) gives
l0
2
ethP2
P1
ethz ~JsTHORN t dlsquo frac14 l0
2
ethP2
P1
~Js s dlsquo frac14 ethU2 U1THORN
(14)
in which the unit vector s frac14 z t is in the plane of the discand normal to the path as shown in Fig 4(b) Now from Eq(14) we see that the total current through any cross sectionof the tube is
I frac14ethP2
P1
~Js s dlsquo frac14 2
l0
ethU2 U1THORN (15)
which is clearly a constantIf two different tubes of current are bounded by equipoten-
tial lines separated by the same increment U the two tubeshave the same total current Thus in Fig 6 all of the tubeswith Un frac14 01 have the same total current From this ob-servation we see that the current density is largest under thepole of the magnet and smallest near the edge of the disc atangles near u frac14 180 Notice that the tubes of current areclosed and the radial component of the surface current iszero at the edge of the disc The closed tubes of current areanalogous to eddies that form around an object in flowingwater hence the name ldquoeddy currentsrdquo (also ldquoFoucaultcurrentsrdquo) Because of the finite conductivity of the disc theeddy currents dissipate energy This energy must be suppliedby the mechanical source turning the axle of the disc
C Faradayrsquos law and the open-circuit voltage
Faradayrsquos law in integral form isthornCethtTHORN
frac12~Eeth~r tTHORN thorn~veth~r tTHORN ~Beth~r tTHORN d~lsquo frac14 d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S
(16)
where we explicitly indicate that the closed contour Cbounding the open surface S can vary with time and ~v isthe velocity for a point on the contour24 We will apply
Eq (16) to the contour ABCDA in Fig 3(a) shown inmore detail in Fig 7
For this contour in the limit u frac14 xt 0 the expres-sion on the left-hand side of Eq (16) becomes
VethqbubTHORN thornethqb
qfrac140
frac12~Eethqub 0THORN thorn~vethqub 0THORN
~Bethqub 0THORN q dq (17)
The integral in Eq (17) is for the portion of the contourCD that is in the disc where the constitutive equation forthe surface current density in the laboratory frame applieswhich is
~JsethqubTHORN ~Jethqub 0THORNd
frac14 rdfrac12~Eethqub 0THORN thorn~vethqub 0THORN ~Bethqub 0THORN(18)
When Eq (18) is substituted into Eq (17) we obtain
VethqbubTHORN thorn1
rd
ethqb
qfrac140
q ~JsethqubTHORNdq (19)
for our final result for the left-hand side of Eq (16)Now consider the expression on the right-hand-side of Eq
(16) for the contour ABCDA In the time increment t thearea S in Fig 7 increases by the increment S (gray in thefigure) We will assume that the applied magnetic field ismuch greater than axial component of the magnetic field dueto the current in the disc (j~Baj jz ~Bij) and we will ignorethe latter Then the time variation in the flux of the magneticfield through S is due to the applied field ~Ba passingthrough S or
d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S frac14 limt0
1
t
ethqb
qfrac140
~BaethqubTHORN ethzTHORNq u dq
264
375 frac14 lim
t0
ut
ethqb
qfrac140
qBaethqubTHORN dq
264
375 frac14 x
ethqb
qfrac140
qBaethqubTHORN dq
(20)
After equating the left-hand- and right-hand-sides of Eq (16) for the contour ABCDAmdashequating Eqs (19) and (20)mdashweobtain the open-circuit voltage at the terminals A-B in Fig 3(a) to be
Fig 7 Details for contour C used with Faradayrsquos law
911 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 911
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13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
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13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
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13023920174 On Sun 24 Aug 2014 212302
where t is a unit vector tangent to the path After taking frac12zEq (4) t and rearranging terms we obtain
~Bi t frac14 l0
2ethz ~JsTHORN t (13)
Substituting Eq (13) into the left-hand side of Eq (12) gives
l0
2
ethP2
P1
ethz ~JsTHORN t dlsquo frac14 l0
2
ethP2
P1
~Js s dlsquo frac14 ethU2 U1THORN
(14)
in which the unit vector s frac14 z t is in the plane of the discand normal to the path as shown in Fig 4(b) Now from Eq(14) we see that the total current through any cross sectionof the tube is
I frac14ethP2
P1
~Js s dlsquo frac14 2
l0
ethU2 U1THORN (15)
which is clearly a constantIf two different tubes of current are bounded by equipoten-
tial lines separated by the same increment U the two tubeshave the same total current Thus in Fig 6 all of the tubeswith Un frac14 01 have the same total current From this ob-servation we see that the current density is largest under thepole of the magnet and smallest near the edge of the disc atangles near u frac14 180 Notice that the tubes of current areclosed and the radial component of the surface current iszero at the edge of the disc The closed tubes of current areanalogous to eddies that form around an object in flowingwater hence the name ldquoeddy currentsrdquo (also ldquoFoucaultcurrentsrdquo) Because of the finite conductivity of the disc theeddy currents dissipate energy This energy must be suppliedby the mechanical source turning the axle of the disc
C Faradayrsquos law and the open-circuit voltage
Faradayrsquos law in integral form isthornCethtTHORN
frac12~Eeth~r tTHORN thorn~veth~r tTHORN ~Beth~r tTHORN d~lsquo frac14 d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S
(16)
where we explicitly indicate that the closed contour Cbounding the open surface S can vary with time and ~v isthe velocity for a point on the contour24 We will apply
Eq (16) to the contour ABCDA in Fig 3(a) shown inmore detail in Fig 7
For this contour in the limit u frac14 xt 0 the expres-sion on the left-hand side of Eq (16) becomes
VethqbubTHORN thornethqb
qfrac140
frac12~Eethqub 0THORN thorn~vethqub 0THORN
~Bethqub 0THORN q dq (17)
The integral in Eq (17) is for the portion of the contourCD that is in the disc where the constitutive equation forthe surface current density in the laboratory frame applieswhich is
~JsethqubTHORN ~Jethqub 0THORNd
frac14 rdfrac12~Eethqub 0THORN thorn~vethqub 0THORN ~Bethqub 0THORN(18)
When Eq (18) is substituted into Eq (17) we obtain
VethqbubTHORN thorn1
rd
ethqb
qfrac140
q ~JsethqubTHORNdq (19)
for our final result for the left-hand side of Eq (16)Now consider the expression on the right-hand-side of Eq
(16) for the contour ABCDA In the time increment t thearea S in Fig 7 increases by the increment S (gray in thefigure) We will assume that the applied magnetic field ismuch greater than axial component of the magnetic field dueto the current in the disc (j~Baj jz ~Bij) and we will ignorethe latter Then the time variation in the flux of the magneticfield through S is due to the applied field ~Ba passingthrough S or
d
dt
eth ethSethtTHORN
~Beth~r tTHORN d~S frac14 limt0
1
t
ethqb
qfrac140
~BaethqubTHORN ethzTHORNq u dq
264
375 frac14 lim
t0
ut
ethqb
qfrac140
qBaethqubTHORN dq
264
375 frac14 x
ethqb
qfrac140
qBaethqubTHORN dq
(20)
After equating the left-hand- and right-hand-sides of Eq (16) for the contour ABCDAmdashequating Eqs (19) and (20)mdashweobtain the open-circuit voltage at the terminals A-B in Fig 3(a) to be
Fig 7 Details for contour C used with Faradayrsquos law
911 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 911
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13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
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13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
VethqbubTHORN frac14 1
rd
ethqb
qfrac140
q ~JsethqubTHORNdqthorn xethqb
qfrac140
qBaethqubTHORN dq frac14 2
l0rd
ethqb
qfrac140
1
qUethqub z frac14 0thornTHORN
udqthorn x
ethqb
qfrac140
qBaethqubTHORN dq
(21)
where in the last line we have substituted Eq (10) for ~JsTo complete the derivation for the open-circuit voltage we must substitute for the magnetic scalar potential Eqs (8) and
(9) and perform the differentiation and integration indicated in Eq (21) For points qbub in each of the three regions shownin Fig 5 the evaluation is different for example for Region I the expression to be evaluated is
VI frac14 2
l0rd
ethqi
qfrac140
1
qUI
udqthorn
ethqo
qfrac14qi
1
qUII
udqthorn
ethqb
qo
1
qUIII
udq
264
375thorn xB0
ethqo
qfrac14qi
qdq (22)
The calculations are straightforward but tedious All of the definite integrals can be evaluated in closed form25 and final resultsfor the open-circuit voltage are
VIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
on q2in cnethqon qinTHORNcosub thorn Fethqin cnubTHORNthornFethqbn cnubTHORN
Fethqon cnubTHORN Fethqbn 1=cnubTHORNg (23)
VIIethqbnubTHORN frac14 xBoa2
2feth1=anTHORN2frac12q2
bn q2in cnethqbn qinTHORNcosub thorn Fethqin cnubTHORN
Fethqbn 1=cnubTHORNg (24)
and
VIIIethqbnubTHORN frac14 xBoa2
2frac12Fethqbn cnubTHORN
Fethqbn 1=cnubTHORN (25)
in which the function F is given by
Fetha bubTHORN frac14 bb acosub
a2 thorn b2 2abcosub
(26)
Figure 8 is a contour plot of the open-circuit voltage normal-ized so that maxjVnj frac14 10 for the case aAfrac14 0170 andcAfrac14 0667 This is the same case as for the magnetic scalarpotential in Fig 6 All of the contours are spaced by the incre-ment Vn frac14 01 except the incomplete contours forVnfrac14 0033 and 005 Notice that the voltage has even symme-try about the lines ub frac14 0 and 1808 It has a maximum at thetop edge of the magnetic pole (qb frac14 cthorn aub frac14 0) and hassmall negative values in the area just above the center of thedisc A comparison of the lines of constant voltage in Fig 8with the streamlines for the current in Fig 6 shows that thetwo sets of lines are orthogonal in Regions I and III wherethere is no applied magnetic field This is the relationship weexpect for an electrically-thin conductor in the quasi-staticlimit We will have more to say about this plot when we dis-cuss Faradayrsquos observations in the next section of the paper
III FARADAYrsquoS OBSERVATIONS
Faraday spent a considerable amount of time experimentingwith his first dynamo A measure of this can be seen in his
diary where he devoted five pages including 23 figures to hisfirst dynamo By comparison he devoted two short paragraphswithout figures to the dynamo shown in Fig 2(b)36 Faradayrsquosmeasurements were made with a galvanometer that hereferred to as ldquoroughly made yet sufficiently delicate in itsindicationsrdquo The instrument could detect a very small currentbut the measurements were qualitative in the sense that
Fig 8 Contour plot for the open-circuit voltage VnethqbubTHORN for the case
aAfrac14 0170 and cAfrac14 0667 The voltage is normalized so that
maxjVnj frac14 10 and the contours are spaced by the increment Vn frac14 01
except the incomplete contours for Vnfrac14 0033 and 005
912 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 912
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13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
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13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
Faraday recorded the deflection of the galvanometer usingterms such as ldquomost stronglyrdquo and ldquoless stronglyrdquo Faradayvaried the arrangement of the elements (brushes magnet etc)in his dynamo to determine the characteristics of the currenthe thought was produced in the disc In this section using theanalysis just discussed we will examine Faradayrsquos observa-tions and his interpretation for them We will assume that ouropen-circuit voltage is proportional to the current that causedthe deflection of Faradayrsquos galvanometer26
Faraday reversed both the direction of rotation of the discand the direction of the applied magnetic field and he sawthat a reversal of either changed the sense of the deflectionof the galvanometer He reduced the applied magnetic fieldby moving one of the poles of the magnet away from thedisc and he saw the deflection decrease These observationsare in agreement with the product xBo appearing in theexpressions for the open-circuit voltage in Eqs (23)ndash(25)
Faraday was able to deduce many of the key features wesee in the contour plot for the open-circuit voltage shown inFig 8 He did this by moving the brushes to different loca-tions on the disc and observing the change in the deflectionof the galvanometer He placed one brush at the center of thedisc (on the axle) and the other brush at symmetrical pointsabout the line ub frac14 0 or 1808 By noting that the deflectionof the galvanometer was the same at the two points hededuced the even symmetry we see for the pattern about thisline With one brush at the center of the disc and the other atthe edge of the disc he varied the angular position of the lat-ter and noticed that the deflection of the galvanometer wasmaximum when the brush was opposite the magnetic pole(ub frac14 0) and decreased as the brush was moved away fromthis point (ub increased) This observation is consistent withwhat we see in Fig 8 for qbfrac14A
Faraday also varied the position of the magnetic poles Forcomparison with his observations we will determine theopen-circuit voltage when the brush in Fig 3(a) is at the topedge of the disc directly above the magnetic poleqb frac14 A ub frac14 0 For this case the open-circuit voltage Eq(23) becomes simply
Vethqb frac14 Aub frac14 0THORN frac14 xB0A2
2etha=ATHORN2 1thorn c=A
1 c=A
(27)
which we have plotted in Fig 9 as a function of polersquos sizeaA and position cA
For any size pole the voltage is maximum when the poleis as far away from the center of the disc as possible whilestill being completely over the disc or when cAfrac14 1 ndash aAIn this position the velocity of the disc relative to the pole ismaximum Also the larger the pole the larger the voltagewith maximum voltage occurring when the diameter of thepole equals the radius of the disc that is aAfrac14 05 andcAfrac14 05 When Faraday lowered the magnetic poles so asto decrease cA he noted that the ldquohellipeffect was the same [aswith the poles raised] and the deflection was very sensiblerdquoThis observation can be explained by the small size ofFaradayrsquos poles They were either square or rectangular inshape and roughly equivalent to circular poles withaAfrac14 00727 Thus his results approximately correspond tothe curve aAfrac14 01 in Fig 9 which in the central region isfairly flat so the variation with cA would have been difficultto detect in his qualitative measurements
From his measurements Faraday was able to show that cur-rent was induced in the conducting disc only when the disc
moved through the magnetic field He concluded that the cur-rent went in the radial direction from the central part of thedisc past the pole to the edge of the disc where itldquodischargedrdquo or returned in the part of the disc on either sideof the pole This description is remarkably similar to what wesee for the distribution of the surface current in Fig 6
Commenting on his first dynamo Faraday said ldquoHeretherefore was demonstrated the production of a permanent[direct or continuous] current of electricity by ordinary mag-netsrdquo28 Thus he fulfilled the goal he stated earlier of makingthe experiment of Arago a new source of electricity Faradaywas confident that he had also found the explanation forAragorsquos rotations which was as follows The magnetic fieldof the needle induced current in the rotating disc this cur-rent in turn created a magnetic field that exerted a force onthe needle causing it to rotate
IV REPEATING FARADAYrsquoS EXPERIMENTS
We repeated some of the experiments Faraday made withhis first dynamo with a two-fold objective in mind First weaim to verify the analysis presented earlier which is basedon Smythersquos approximation for the magnetic scalar potentialand second we provide quantitative results that supportFaradayrsquos qualitative observations Concerning the firstobjective we followed Faradayrsquos advice that ldquoNothing is asgood as an experiment which whilst it sets error right givesan absolute advancement in knowledgerdquo29
Figures 10(a) and 10(b) are schematic drawings for the ex-perimental model which is very similar to Faradayrsquosdynamo except that it is constructed from modern materialsThe circular copper disc of radius Afrac14 750 cm and thicknessdfrac14 086 mm was mounted on a brass axle The axle washeld in the chuck of a drill press and the speed of rotation ofthe disc which was measured with an optical tachometerwas varied by adjusting the beltstepped-pulley system of thedrill press The magnetic field was that of two neodymiumpermanent magnets (K amp J Magnetics Inc DX08) of radiusamfrac14 127 cm and length 127 cm bonded to the ends of ayoke formed from laminated steel sheets The purpose of theyoke was to direct the return field of the magnets to an areaoff the disc so that the only magnetic field applied to the discwas that between the poles Figure 10(c) is a graph of the
Fig 9 Open-circuit voltage as a function of the polersquos size aA and position
cA when the brush is at the top edge of the disc directly above the magnetic
pole at qb frac14 A ub frac14 0 The voltage is normalized so that maxjVnj frac14 10
which occurs for aAfrac14 05 cAfrac14 05 For all points on the graph the pole is
completely over the disc
913 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 913
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13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
magnetic field measured on the horizontal plane centeredbetween the poles of the permanent magnets The points onthis graph are averages of measurements made along threedifferent radial lines from the center of the poles The mag-netic field is seen to have a maximum value of about 108 Tat the center of the poles (ramfrac14 00) to decrease to abouthalf this value at the edges of the poles (ramfrac14 10) and torapidly decay beyond this point
The disc was connected to the external circuit by spring-loaded carbon brushes of diameter 46 mm [see Fig 10(b)]
One brush was at the center of the disc and a pair of opposingbrushes located on opposite sides of the disc and connected inparallel could be moved to various positions (qb ub) on thedisc Wires embedded in the brushes were soldered directly tothe external circuit where the open-circuit voltage V wasmeasured with a digital voltmeter The good electrical contactbetween the spring-loaded brushes and the disc resulted invery little fluctuation of the voltage as the disc rotated
One complication arose in the comparison of the theorywith the measurements The magnetic field for the theory isuniform over the area of the poles whereas the magneticfield in the experiment varies with the radial distance fromthe center of the poles To make the comparison we definedan effective radius ae for the poles used in the experimentwhich is the radius of fictitious poles with uniform magneticfield equal to Bz(rfrac14 0) that produce the same total flux as theactual poles Mathematically we express this as
pa2eBzethr frac14 0THORN frac14 2p
eth3am
rfrac140
BzethrTHORNrdr (28)
or
ae frac14 am
2
eth3am
rfrac140
BzethrTHORNrdr
a2mBzethr frac14 0THORN
26664
37775
1=2
(29)
When Eq (29) was applied to the results in Fig 10(c) thevalue aefrac14 102am was obtained A value of ae this close toam implies that the additional magnetic field outside of thepoles in Fig 10(c) just compensates for the reduction in themagnetic field under the poles For comparison of theoreticalcalculations with measurements the value ae was used for ain the theory
In all of our measurements the magnetic poles were locatedat cAfrac14 0663 and aeAfrac14 0173 These values are roughly thesame as those used in the earlier calculations For the firstmeasurement the brush was placed above the magnetic polesnear the edge of the disc (qb=A frac14 0951 ub frac14 0) and theangular speed of the disc was varied The theoretical results(curve) for the open-circuit voltage V versus angular speed xare compared with the measured results (dots) in Fig 11 The
Fig 10 Details for the experimental model which is similar to Faradayrsquos
first dynamo (a) Side view in which the brushes and external circuit are not
shown (b) Front view showing the brushes and external circuit (c) Graph of
the magnetic field measured on the horizontal plane centered between the
poles of the permanent magnets The points on the graph are the average of
measurements made along three different radial lines from the center of the
poles
Fig 11 Comparison of theoretical and measured results for the open-circuit
voltage V versus the angular frequency x with qb=A frac14 0951 ub frac14 0
(aeAfrac14 0173 and cAfrac14 0663)
914 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 914
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
theory and measurement are seen to be in good agreement andboth exhibit a linear dependence on x as expected
In the next set of measurements the angular speed of thedisc was fixed at 772 rpm and the position of the brush(qb ub) was moved over different paths on the surface ofthe disc much as Faraday did in his experimentsRepresentative results from these experiments which meas-ured the open-circuit voltage V versus position are shown inFig 12 In Fig 12(a) the radial position of the brush is fixed(qbAfrac14 0960) while the angular position ub is varied and inFig 12(b) the angular position for the brush is fixed(ub frac14 45) while the radial position qb is varied In bothcases the theory (curve) and measurement (dots) are againin good agreement Notice in Fig 12(b) that both the theoret-ical and measured results show the voltage becoming slightlynegative for qb=A lt 04
V DISCUSSION WHAT EVER BECAME OF
FARADAYrsquoS FIRST DYNAMO
In our study we wondered what became of Faradayrsquos firstdynamo and if his machine could be of use today The an-swer to this question is fairly simple As we saw from ouranalysis eddy currents are produced in the disc even when
no current is being drawn from the machine These eddy cur-rents dissipate significant energy and make the machineimpractical as a source of electric power This point is nicelyillustrated by considering the open-circuit voltage on theleft-hand side of Eq (21) to be composed of the two termson the right-hand side of this equation V frac14 Vi thorn Vs Thevoltage Vi is due to the current in the disc and can be thoughtof as the voltage produced by the surface current ~Js passingthrough the resistance of a strip of conductor of unit widthThe voltage Vs represents a source due to the applied mag-netic field traditionally called the ldquoelectromotive forcerdquo(emf) In Fig 13 the three terms V Vi and Vs (normalized sothat jVnjmax frac14 10) are shown as a function of the positionqbA along the radial line ub frac14 0 This line starts at the cen-ter of the disc passes under the pole and ends at the topedge of the disc The emf (Vsn) increases on the portion ofthe path that is under the pole and reaches a maximum ofabout Vsnfrac14 25 The voltage Vin due to the current is alwaysnegative so it subtracts from the emf making the open-circuit voltage drop to only Vnfrac14 08 at the top edge of thedisc Thus the eddy currents in the disc reduce the voltageavailable from the machine to about one-third of the emf
The inefficiency of the dynamo was also evident in themeasurements discussed in Sec IV When the disc wasrotated between the poles of the magnet a strong force resist-ing the motion was felt a consequence of Lenzrsquos law30
There was also a noticeable increase in the temperature ofthe rotating disc In a period of about one minute the tem-perature of the disc rotating at 772 rpm increased from theambient value of 246 8C (763 8F) to about 680 8C (154 8F)The energy that raises the temperature of the disc must besupplied by the mechanical source turning the axle of thedisc
Symmetric designs for the dynamo such as the one shownin Fig 2(b) do not suffer from the same problem with eddycurrents as the asymmetric design Analysis of the com-pletely symmetric structure shows that there is no conductioncurrent in the disc when the terminals are left open Andeven when current is drawn by the external circuit the cur-rent in the disc is in the radial direction that is when noeddies are formed13ndash16 Hence most attempts to make apractical unipolar or homopolar generator have used sym-metric structures These generators produce a high current at
Fig 12 Comparison of theoretical and measured results for the open-circuit
voltage V versus the position of the brush qb ub (a) Radial position fixed at
qbAfrac14 0960 while angular position is varied (b) Angular position fixed at
ub frac14 45
while radial position is varied (In both cases aeAfrac14 0173
cAfrac14 0663 and xfrac14 772 rpm)
Fig 13 The open-circuit voltage V voltage due to the current in the disc Vi
and source voltage (emf) Vs versus qbA for the radial line ub frac14 0 All of
the voltages are normalized so that maxjVnj frac14 10 and all of the parameters
are the same as those for Fig 8
915 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 915
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
a low voltage and the loss due to the current passing throughthe resistance of the brushes is of concern To lower this re-sistance some designs incorporate mercury or a liquid metal-lic alloy in the brushes as Faraday did albeit with moresophisticated designs than Faradayrsquos simple contacts31
Commercial use of even the symmetric designs has been lim-ited to very specialized applications32
The eddy-current disc brake is a structure very similar toFaradayrsquos first dynamo with the permanent magnet inFaradayrsquos design replaced by an electromagnet The conduct-ing disc is mounted on an axle that normally rotates Whenthe rotation is to be slowed or stopped the electromagnet isactivated and the kinetic energy taken from the rotationalmotion of the axle is dissipated by the eddy currents in thedisc The applications of this technology are diverse and rangefrom the brakes on the famous Japanese Shinkansen (bullettrain) to providing resistance to motion in fitness equipmentsuch as rowing machines33 The analysis for the eddy-currentdisc brake is similar to that for the Faraday disc only the em-phasis is usually on obtaining the torque on the axle versusvarious parameters such as the angular frequency and themagnetic flux34ndash37 The calculation we have used fromSmythersquos paper was originally intended for obtaining the tor-que17 In Europe linear versions of the eddy-current brake arebeing tested for railway applications38 In these devices themagnetic field is generated by a linear array of electromagnetson the car and applied to the rail The eddy currents producedin the rail slow the car and heat the rail A section of the rail isheated only as the car passes so the heating is not as severe asfor the disc brake which is heated continuously as long as thebrake is energized
As with the more common friction brakes all eddy-current brakes convert kinetic energy into heat This is unde-sirable in applications in which energy conservation is ofconcern For these applications electromagnetic regenerativebraking may be a better option Regenerative braking is usedin electric and hybrid (gasolineelectric) automobilesBatteries are used to power electric motors that propel theautomobile and when the automobile is to be slowed orstopped these motors are used as generators to charge thebatteries Thus a portion of the kinetic energy of the auto-mobile is recovered and stored for future use
The experiments Faraday made with his first dynamo gavehim insight into electromagnetic induction and among otherthings allowed him to give the first correct explanation forwhat caused Aragorsquos rotations The dynamo in its originalform was not a prototype for a practical source of electricpower However from the historical record it is clear thatFaradayrsquos first dynamo was an important step in the develop-ment of modern generators39 The fundamental principles hediscovered with his dynamo were quickly applied by othersto produce efficient generators
ACKNOWLEDGMENTS
The author would like to thank his Georgia Tech col-leagues Professors Waymond Scott Jr John Buck (bothfrom ECE) and Andrew Zangwill (Physics) for their sugges-tions for improving the manuscript
a)Electronic mail glennsmithecegatechedu1M Arago ldquoLrsquoaction que les corps aimantes et ceux qui ne le sont pas exer-
cent les uns sur les autresrdquo Ann Chim Phys 28 325 (1825) and M
Arago ldquoNote concernant les phenomenes magnetiques auxquels le
mouvement donne naissancerdquo ibid 32 213ndash223 (1826) An account in
English is in C Babbage and J F W Herschel ldquoAccount of the repetition
of M Aragorsquos experiments on magnetism manifested by various substan-
ces during the act of rotationrdquo Philos Trans Roy Soc London 115
467ndash496 (1825)2M Faraday Experimental Researches in Electricity Vol I (Taylor and
Francis London 1839 Republication Green Lion Santa Fe NM 2000)
Paragraph 83 pg 253M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraphs 99ndash136 pp 381ndash3864M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraphs 83ndash100 pp 25ndash29 and 119ndash134 pp
34ndash395S P Thompson Michael Faraday His Life and Work (Cassell London
1901 Republication Elibron Classics New York 2004) pg 1236M Faraday Faradayrsquos Diary edited by T Martin (G Bell and Sons
London 1932) Vol I Paragraph 228 pg 3977M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 155 p 468R J Stephenson ldquoExperiments with a unipolar generator and motorrdquo
Am J Phys 5 108ndash110 (1937)9J W Then ldquoLaboratory experiments in motional electric fieldsrdquo Am J
Phys 28 557ndash559 (1960)10J W Then ldquoExperimental study of the motional electromotive forcerdquo
Am J Phys 30 411ndash415 (1962)11M J Crooks D B Litvin P W Matthews R Macaulay and J Shaw
ldquoOne-piece Faraday generator A paradoxical experiment from 1851rdquo
Am J Phys 46 729ndash731 (1978)12R D Eagleton ldquoTwo laboratory experiments involving the homopolar
generatorrdquo Am J Phys 55 621ndash623 (1987)13H H Woodson and J R Melcher Electromechanical Dynamics Part I
Discreet Systems (Wiley New York 1968) pp 286ndash28914J Van Bladel Relativity and Engineering (Springer-Verlag Berlin 1984)
pp 283ndash29115J Van Bladel ldquoRelativistic theory of rotating disksrdquo Proc IEEE 61
260ndash268 (1973)16H Montgomery ldquoCurrent flow patterns in a Faraday discrdquo Eur J Phys
25 171ndash183 (2004)17W R Smythe ldquoOn eddy currents in a rotating diskrdquo Trans AIEE 61
681ndash684 (1942)18W R Smythe Static and Dynamic Electricity 3rd ed (McGraw-Hill
New York 1968) pp 390ndash39319This type of problem is sometimes referred to as a ldquoquasi-static magnetic
field systemrdquo and it is discussed in detail in H H Woodson and J R
Melcher Electromechanical Dynamics Part I Discreet Systems (Wiley
New York 1968) pp 6ndash8 260ndash264 270ndash277 284ndash289 B19ndashB2520In the local rest frame for a point on the disc the thickness of the disc is
assumed to be much less than the skin depth in the conductor In this
frame the volume current density is then practically uniform throughout
the thickness of the disc In the quasi-static approximation the volume
current density is the same in the moving frame and in the laboratory
frame hence it is practically uniform in the laboratory frame21A I Borisenko and I E Tarapov Vector and Tensor Analysis with
Applications translated by R A Silverman (Prentice-Hall Englewood
Cliffs NJ 1968) pp 211ndash22322Smythe solves for the stream function U which is simply related to the
magnetic scalar potential UethquTHORN frac14 eth2=l0THORNUethqu z frac14 0thornTHORN His method
is briefly as follows First he considers a pole placed over an infinite con-
ducting sheet The radius of the pole is a and it is offset from the origin by
c He obtains an integral for the stream function U1 of this pole and he
evaluates this integral approximately Next he introduces a second pole
with the same total flux as the first pole but of opposite sign and he obtains
the approximate stream function U2 for this pole The radius and offset
from the origin for the second pole are ~a and ~c with ~c ~a gt A Finally
he adjusts ~a and ~c to make the superposition Ufrac14U1thornU2 satisfy the
boundary condition Ufrac14 0 at the radius qfrac14A (edge of the disc)23Normally a tube of current is a region of three-dimensional space
delineated by a side surface that is everywhere parallel to the direction of
the volume current density ~J The total current I passing through any
cross-sectional area of the tube is the samemdashthink of a pipe with the water
flowing through the pipe representing the current Here we are using the
two-dimensional version of the tube of current The current is on a surface
(on the disc) and the sides of the tube are two lines that are everywhere
parallel to the direction of the surface current density ~Js The total current
916 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 916
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302
I passing through any cross-sectional contour joining these lines is the
same24H Gelman ldquoFaradayrsquos law for relativistic and deformed motion of a
circuitrdquo Eur J Phys 12 230ndash233 (1991)25I S Gradshteyn and I M Ryzhik Tables of Integrals Series and
Products 7th ed (Academic New York 2007)26The deflection of the galvanometer is a function of the current through it
If the internal resistance of the disc is always small compared to the resist-
ance of the external circuit this current exhibits the same proportionality
to the open-circuit voltage for all positions of the brush (qb ub)27This equivalence is based on equating the area for a circular pole to that
for the square or rectangular pole28M Faraday Experimental Researches in Electricity (Taylor and Francis
London 1839) Vol I Paragraph 90 p 2729S P Thompson Michael Faraday His Life and Work (Cassell London
1901) pg 27630W M Saslow ldquoMaxwellrsquos theory of eddy currents in thin conducting
sheets and applications to electromagnetic shielding and MAGLEVrdquo Am
J Phys 60 693ndash711 (1992)31D A Watt ldquoThe development and operation of a 10-kW homopolar gen-
erator with mercury brushesrdquo Proc IEE (London) 105A 233ndash240 (1958)
32A I Miller ldquoEssay 3 Unipolar Induction a Case Study of the
Interaction between Science and Technologyrdquo in A I Miller Frontiersof Physics 1900ndash1911 Selected Essays (Birkheuroauser Boston 1986) pp
153ndash18733A Mochizuki ldquoA new series of the Shinkansen EMU train made its
debutrdquo Jpn Railw Eng 25 6ndash11 (1985)34H D Wiederick N Gauthier D A Campbell and P Rochon ldquoMagnetic
braking Simple theory and experimentrdquo Am J Phys 55 500ndash503
(1987)35M A Heald ldquoMagnetic braking improved theoryrdquo Am J Phys 56
521ndash522 (1988)36M Marcuso R Gass D Jones and C Rowlett ldquoMagnetic drag in the
quasi-static limit Experimental data and analysisrdquo Am J Phys 59
1123ndash1129 (1991)37J M Aguirregabiria A Hernandez and M Rivas ldquoMagnetic braking
revisitedrdquo Am J Phys 65 851ndash856 (1997)38J Schykowski ldquoEddy-current braking A long road to successrdquo http
wwwrailwaygazettecomnewssingle-viewvieweddy-current-braking-a-
long-road-to-successhtml (2008)39S P Thompson Polyphase Electric Currents and Alternate-Current
Motors 2nd ed (Spon and Chamberlain New York 1900) pp 421ndash471
917 Am J Phys Vol 81 No 12 December 2013 Glenn S Smith 917
This article is copyrighted as indicated in the article Reuse of AAPT content is subject to the terms at httpscitationaiporgtermsconditions Downloaded to IP
13023920174 On Sun 24 Aug 2014 212302