experimental methods in marine dynamics
TRANSCRIPT
-
7/23/2019 Experimental Methods in Marine Dynamics
1/182
_______________________________________________________________________________________________________________
FAKULTET FOR INGENIRVITENSKAP OG TEKNOLOGI NTNU TRONDHEIMNORGES TEKNISK-NATURVITENSKAPELIGE UNIVERSITET
FACULTY OF ENGINEERING SCIENCE AND TECHNOLOGY NTNU TRONDHEIMNORWEGIANUNIVERSITY OF SCIENCE AND TECHNOLOGY
_______________________________________________________________________________________________________________
TMR7
Experimental Methods in
Marine Hydrodynamics
Sverre Steen
Revised August 2014
MARINTEKNISK SENTER INSTITUTT FOR MARIN TEKNIKKMARINE TECHNOLOGY CENTRE DEPARTMENT OF MARINE TECHNOLOGYTRONDHEIM, NORWAY
-
7/23/2019 Experimental Methods in Marine Dynamics
2/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page1
CONTENTS
1 INTRODUCTION..................................................................................................31.1 Background...............................................................................................................................3
1.2 Whymodeltests.......................................................................................................................4
2 GENERALMODELLINGLAWS..............................................................................62.1 Geometricalsimilarity..............................................................................................................6
2.2 Kinematicsimilarity..................................................................................................................6
2.3 Dynamicsimilarity....................................................................................................................7
2.4 ScalingRatios..........................................................................................................................10
2.5 Hydroelasticity........................................................................................................................11
2.6 Cavitation................................................................................................................................13
3 EXPERIMENTALFACILITIES...............................................................................143.1 Introduction............................................................................................................................14
3.2 TowingTanks..........................................................................................................................14
3.3 CavitationTunnel....................................................................................................................18
3.4 OceanLaboratories.................................................................................................................20
3.5 Generationofenvironment....................................................................................................21
4 INSTRUMENTATION.........................................................................................284.1 Generaldescriptionofequipment.........................................................................................28
4.2 Strainanddisplacementmeasurements................................................................................28
4.3 Positionmeasurements..........................................................................................................32
4.4 Accelerations..........................................................................................................................34
4.5 PressureTransducers..............................................................................................................35
4.6 Velocities................................................................................................................................38
4.7 Forcemeasurements Dynamometers..................................................................................41
4.8 WaveMeasurements..............................................................................................................42
4.9 DataAcquisition......................................................................................................................44
4.10 SamplingFrequency...............................................................................................................48
4.11 LengthofRecords...................................................................................................................50
4.12 Calibration..............................................................................................................................53
4.13 Zeroing....................................................................................................................................54
5 PHYSICALMODELLING......................................................................................555.1 General...................................................................................................................................55
5.2 RigidModels...........................................................................................................................55
5.3 ElasticModels.........................................................................................................................57
6 CONVENTIONALSHIPTESTING.........................................................................616.1 General...................................................................................................................................61
6.2 Towingandpropulsiontestsintowingtank..........................................................................61
6.3 Cavitationtunneltests............................................................................................................65
6.4 Maneuveringtests..................................................................................................................67
7 SEAKEEPINGTESTING.......................................................................................717.1 General...................................................................................................................................71
-
7/23/2019 Experimental Methods in Marine Dynamics
3/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page2
7.2 TestRequirement...................................................................................................................71
7.3 Testsetup..............................................................................................................................72
7.4 TestProcedure........................................................................................................................73
7.5 Tankwalleffects.....................................................................................................................75
8 OFFSHORESTRUCTURETESTING......................................................................77
8.1 General...................................................................................................................................77
8.2 TestRequirements..................................................................................................................77
8.3 Deepwaterstructuresrequirements.....................................................................................78
8.4 TestProcedure........................................................................................................................80
9 REALTIMEHYBRIDMODELTESTING................................................................829.1 Testingoffloatingoffshoreshipsandplatformswithmooringandflexiblerisersystems...83
9.2 Testingofhydrofoilships........................................................................................................83
9.3 Testingoffloatingoffshorewindturbines.............................................................................83
9.4 Challengesinhybridmodeltesting........................................................................................83
10 ANALYSISOFMEASUREDDATA........................................................................8510.1 General...................................................................................................................................85
10.2 Statictests..............................................................................................................................85
10.3 Decaytest...............................................................................................................................85
10.4 RegularWaveTest..................................................................................................................88
10.5 IrregularWaveTest................................................................................................................91
11 FULLSCALEMEASUREMENTS.........................................................................10311.1 Deliverytrials........................................................................................................................103
11.2 Shipmonitoringsystems......................................................................................................110
12 ERRORANALYSIS............................................................................................11312.1 Introduction..........................................................................................................................113
12.2 Uncertaintyanalysis.............................................................................................................113
12.3 DiscussionofErrorSources..................................................................................................119
13 MODELTESTSVSNUMERICALCALCULATIONS..............................................12713.1 General.................................................................................................................................127
13.2 ModeltestsforValidationofNumericalCalculations..........................................................128
14 REFERENCES...................................................................................................130
15 INDEX.............................................................................................................132
ANNEXA ExampleofReportingfromModelTest
ANNEXB ExampleofModelTestSpecification
ANNEXC ViscousSurgeDampingofFloatingProductionVesselMooredatSea
ANNEXD ErrorAnalysisofExperiments.LecturenotebyS.Ersdal
ANNEXE ITTCstandardforpoweringperformanceprediction
-
7/23/2019 Experimental Methods in Marine Dynamics
4/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page3
1 INTRODUCTION
ThiscompendiumhasbeenpreparedforthecourseExperimentalMethodsinMarine
Hydrodynamics.Partsofthenotesarebasedonearlierlecturenoteswithinthisfield;seeHuse
(1999)andWalderhaug(1983).ExtensiverevisionsofthecompendiumwrittenbyAarsnesin2001
weremade
by
Steen
in
2004,
2005,
and
2006,
followed
by
smaller
revisions
in
2010
and
2012.
AlthoughthenameofthiscourseisExperimentalMethodsinMarineHydrodynamics,wewill
mainlybetalkingaboutmodeltesting,sincemostexperimentsinmarinehydrodynamicsaremade
inmodelscale.Also,modeltestinginvolvesmanyinterestingissues,likescalingandmodelling.Full
scaletestingishandledasaspecialcase,seechapter11.
Throughoutthetext,manyreferencesaregiventosupplementaryliterature,anditis
recommendedtoconsultthoseforamoreindepthtreatmentofspecialtopics.Agoodtextbook
thatcoversmostofthetopicsintheselecturenotesatanintroductorybutstillmorethoroughlevel
isthebookbyDunn(2005).
Figure 1.1Model tests in Peerlesspool in London in 1761
1.1 Background
Experimentalfacilities
for
model
testing
of
ships
have
along
tradition.
Improved
resistance
performanceoftheshipswasearlythemaindrivingforcebehindthedevelopmentofshipmodel
-
7/23/2019 Experimental Methods in Marine Dynamics
5/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page4
testing.ItisknownthatLeonardodaVinci(aboutyear1500)carriedouttestswith3models
ofships,allwithequallength,butwithdifferentforeandaftshape.Basedonhisexperimentshe
wasabletogiverecommendationaboutwhichshapegivesthehighestspeed.LaterSamuelFortey
(16221651)alsodidtestswithshipmodelsandin1721EmanuelSwedenborggaveadetailed
proposalforshipmodeltestingintroducingtheprinciplewithfallingweightfortowingofthe
models.Inthiswayhewasabletoachieveaknownandconstanttowingforce. In1761thisprinciplewasusedinPeerlesspoolinLondonasshownonthepicturegiveninFigure1.1.Atthat
timenoscalinglawswereavailabletopredictfullscalebehaviourandonehadtoassumethatthe
winnerwasthebestalsoinfullscale.
WilliamFroude(18101879)isoftengiventhehonourforthemethodofreallyusingmodeltesting
forshipdesignbythedevelopmentofamethodforscalingfrommodelresistancetotheactualship
resistance.Thismayberight,butseveralotherworksfromthesametimealsocontribute
significantlytothisdevelopment.Theestablishingofthescalingmethodsshouldthereforemorebe
regardedasaresultoftheincreasinginterestandactivitieswithinthisfield.
FroudestowingtankwasbuiltinSouthEnglandinca1870andisregardedasthebeginningof
modernmodeltesting.ThemaindimensionofthetankwasLxBxd=85mx11mx3m.Itwas
equippedwitharailintheroof,whichcarriedthedynamometers.Maximumspeedwas5m/s.
Shortlyafterthistankwasestablished,severalothertankswerebuiltinEngland,Germanyand
elsewhere.ThetowingtankinTrondheimwascompletedin1939withdimensionLxBxd=170mx
10.5mx5m,whichwasanormaltanksizeatthattime.
Later,thedevelopmentwithinshiptechnologyhasinitiateddevelopmentandbuildingof
specialisedfacilitiesascavitationtunnels,manoeuvringandseakeepingbasins.Duringthelast20
25yearstheneedsfromtheoffshoreindustryhavepushedthisdevelopmentevenfurther,and
complexlaboratorieswiththepossibilityoftestingstructuresinrealisticconditionsincludingwind,
currentaswellasmultidirectionalwaves,havebeenbuilt.Anexampleofthistypeoflaboratoryis
theOceanBasinatMARINTEK.
Differenttypesoffacilitiesaredescribedinmoredetailsinchapter3.
Afurtherdescriptionandreviewofthehistoryanddevelopmentofshipmodeltestingcanbefound
inSNAME(1967)andinStoot(1959)
1.2 Whymodeltests
Hydrodynamicmodeltestingwillbasicallyhavethreedifferentaims:
1. Toachieverelevantdesigndatatoverifyperformanceofactualconceptsforshipsand
othermarinestructures
2. Verificationandcalibrationoftheoreticalmethodsandnumericalcodes
3. Toobtainabetterunderstandingofphysicalproblems.
Alltheaimscanbeassociatedtotheoftenverycomplicatednatureofproblemsconnectedtothe
interactionbetweenfixedandfloatingstructuresandthemarineenvironment.
Aim1isspeciallythecaseiftheanalysisisverycomplicatedforwhichverifiednumericaltoolsare
notavailable.Modeltestcanbeusedtoinvestigateeffectsofsimplificationsusedasbasisfor
-
7/23/2019 Experimental Methods in Marine Dynamics
6/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page5
analyticalornumericalmodels.Inthiswaymodeltestresultscanbeusedtoassist
developmentofmorereliablenumericaltools.
-
7/23/2019 Experimental Methods in Marine Dynamics
7/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page6
2 GENERALMODELLINGLAWS
Physicalmodelsareintendedtorepresentthefullscalesystemascloseaspossibleata(much)
smallerscale.Tobeabletodeterminetheproperpropertiesofthemodelweneedmodellingor
scalinglawsthatensureasimilarbehaviourinmodelandfullscale.
Dimensionalanalysiscanbeusedtoderiveagroupofmeaningfuldimensionlessquantitiesfor
applicablevariables.Thisisparticularlyusefuliftheproblemiscomplex.Typicallyallthevarious
quantitiesassumedtobeofimportanceforacertainphenomenaislisted.Afunctionalrelationship
betweenthedifferentparametergroupsisthenestablishedforallflowgoverningquantities.The
scalinglawsareobtainedbytakingtheratioofthedifferentforces. Adetaileddescriptionof
dimensionalanalysiscanbefoundinTaylor(1974).Aderivationofthemostcommon
dimensionlessvariablesusedinfluiddynamics,usingBuckinghamsPitheoremisfoundinchapter5
ofWhite(2005).
Toachievesimilarityinforcesbetweenthemodelscaleandfullscalesituationthefollowing
conditionsmustbefulfilled:
Geometricalsimilarity
Kinematicsimilarity
Dynamicsimilarity
Inthefollowingtheserequirementswillbediscussed.Amorecomprehensivediscussionabout
modellawsisgivenbyChakrabarti(1998)
2.1 Geometricalsimilarity
Geometricalsimilarstructuresinmodelandfullscalehavethesameshape.Thismeansthata
constantlengthscalebetweenthemexist:
/F ML L
whereLMandLFareanydimensionsofthemodel/fullscalestructure.Therequirementtoequal
lengthratioforalldimensionsdoesnotapplyonlytothestructures,butalsotothesurrounding
environment.Atthefirstviewthisseemstobeaneasyrequirementtosatisfyforpracticaltesting.
Howeverthisneednotbetheactualsituation.Forexampletheactualsurfaceroughnessofaship
cannotbeaccuratelymodelled.Anotherexampleisthealmostunrestrictedextentofthe
surroundingwaterforasailingship(exceptforwaterdepthinsomecases).Thissituationisnot
possibletoreproduceinmodelscale,whichimpliesthatphysicalboundariesalwayspresentin
modeltestingcaninfluencethetestresults.
2.2 Kinematicsimilarity
Theratiosbetweenvelocitiesinmodelscalehavetobeequaltothecorrespondingratiosinfull
scale.Thisimpliesthatflowwillundergothegeometricalsimilarmotionsinbothcases.Asan
exampletheratiobetweentheforwardspeedofashipandtherotationalspeedofthepropeller
hastobethesame:
-
7/23/2019 Experimental Methods in Marine Dynamics
8/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page7
(2 ) (2 )
F M
F F M M
V V
n R n R
or
F MF M
F F M M
V VJ J
n D n D
whereVistheshipspeed,nistherateofrevolutionofthepropeller,Risthepropellerradius,Dis
thepropellerdiameterandJistheadvancecoefficient.
2.3 Dynamicsimilarity
2.3.1 Forces
Dynamicsimilarityisachievedifwehavethesameratioatmodelscaleandfullscaleforthe
differentforcecontributionspresentintheproblem.Inprinciplethefollowingforcecontributions
willbeofimportance:
1. InertiaForces,Fi
2. Viscousforces,Fv
3. Gravitationalforces,Fg
4. Pressureforces, Fp
5. Elasticforcesinthefluid,Fe.
6. Surfaceforces,Fs.
Inaddition,forelasticmodelstheelasticrelativedeformationsmustbeidenticalinmodelandfull
scale.
Wewillusethefollowingdifferentphysicalquantitiestocharacterisethedifferentforce
contributions;physicallength;L,velocity;U,fluiddensity;,gravitationalacceleration;g,andthe
fluidviscositycoefficient;.ThefollowingdependenceofthephysicalparametersL,U,,gand
willexistforthedifferentforcecontributions:
InertiaForces:
2233
LULdt
dx
dx
dU
Ldt
dU
Fi
ViscousForces: ULLdx
dUFv
2
GravitationalForces:3
gLFg
PressureForces:2
pLFp
ElasticfluidForces:2LEF vve
SurfaceForces: LFs
-
7/23/2019 Experimental Methods in Marine Dynamics
9/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page8
wherevistherelativeelongation(compression),Evisthevolumeelasticityandisthesurfacetension.
2.3.2 FroudeNumber
Thedynamicsimilarityrequirementappliedontheratiobetweeninertiaandgravityforcesgives
thefollowingrelation:
gL
U
gL
LU
F
F
g
i
2
3
22
Appliedonmodelandfullscalethisrequirementgives:
2 2
M F
M F
M FN
M F
U U
gL gL
U UF
gL gL
whereFNistheFroudenumber.Geometricalandkinematicsimilarity,andequalityinFroude
numberinmodelandfullscalewillthereforeensuresimilaritybetweeninertiaandgravityforces.
Sincesurfacewavesaregravitywaves,thisimpliesthatequalityinFroudenumbershouldgive
equalityinwaveresistancecoefficient.
2.3.3 ReynoldsNumber
Equalratiobetweeninertiaandviscousforceswillgive:
2 2
i
v
F U L UL UL ReF UL
whereReistheReynoldsnumberand=/ isthekinematicviscosity.EqualityinReynolds
numberbetweenfullscaleandmodelscalewillthereforeensurethattheviscousforcesare
correctlyscaled.
2.3.4 Machsnumber
Theelasticityofwaterwillinfluencethepressuretransmissioninwaterandwillthereforebe
importantforsometypeofmodeltesting.Equalratiobetweeninertiaandelasticforcesgives:
2
22
LE
LU
F
F
vve
i
Usingthegeometricalsimilarityrequirementthatvareequalinmodelandfullscalethis
requirementgives:
2 2 2 2
2 2
, ,
v v v vM F
M F
n
v M v F
U L U L
E L E L
U U
ME E
-
7/23/2019 Experimental Methods in Marine Dynamics
10/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page9
whereMnistheMachnumberand vE isthespeedofsoundinwater.
2.3.5 Webersnumber
Theratiobetweeninertiaandsurfacetensionforcesisgivenfrom:
LU
L
LU
F
F
s
i222
Similarityrequirementforthisforceratioinmodelandfullscalewillnowgivethefollowing
requirement:
2 2
M F
U L U L
whichgives:
( ) ( )
M Fn
M F
M F
U UW
L L
whereWnistheWebersnumber
-
7/23/2019 Experimental Methods in Marine Dynamics
11/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page10
2.4 ScalingRatios
Thefollowingdimensionlessquantitiesarecommonlyusedfortestingofshipandoffshore
structures:
Symbol DimensionlessNumber ForceRatio Definition
Re ReynoldsNumber Inertia/Viscous UL
FN FroudeNumber Inertia/GravityU
gL
Mn MachsNumber Inertia/ElasticityV
U
E
Wn WebersNumber Inertia/SurfacetensionU
L
St Strouhallnumber vf D
U
KC KeuleganCarpenterNumber Drag/Inertia AU T
D
TheStrouhalNumberisnotderivedfromaforceratio.fvisthevortexsheddingfrequencyandStis
thenondimensionalvortexsheddingfrequency,whichagaindeterminetheoscillationfrequency
ofthetransverseliftforcesactingonacylinderwithcrossdimensionD.
TheKeuleganCarpenterNumberisdeterminedfromforceratiobetweendragandinertiaforces
forthecasewithoscillatingflowpastacylinder.TistheperiodofoscillationandUAisthevelocity
amplitude.EqualKCinmodelandfullscaleisforexampleachievedifthesameratiobetweenwave
heightandcylinderdiameterisused.
Inpracticaltestingitwillnotbepossibletosatisfysimultaneouslythedifferentscalinglaws.For
exampleshipsandoffshorestructuresareformostpracticalsituationinfluencedbysurfacewave
effects,eitherfromincomingwavesorwavegeneratedbytheforwardspeedormotionsofthe
structure.Gravitationalforceswillgovernthesurfacewaveformation.Thisimpliesthatforthese
conditionsequalityinFroudenumberinmodelandfullscalemustbeachieved.Ifviscousforcesare
importantfortheactualsituation,therequirementofequalityinReynoldsnumbershouldin
principlealsobesatisfied.Thisisnotpossibletoachieve.Theviscousforceswillnotbecorrectly
scaledandinthescalingprocessfrommodeltofullscalethiseffecthastobeevaluated.
OtherpracticallimitationsforachievingequalityinRearemodelsizeandnecessarymodelspeed.
TherequirementofconstantUL(assumingconstant)willformostcasesbeimpossibletoachieve.
Inconventionalmodeltestingofshipsandoffshorestructures,physicalscalingandtestexecution
aremostcommonlycarriedoutbasedonFroudeScaling.TheeffectofdifferentReynoldsnumberis
accountedforbydifferentscalingprocedures.Atypicalexampleisshipresistancetests,where
scalingmethodsforcorrectingforeffectofdifferentReynoldsnumberiswellestablished.Forother
applicationsnoestablishedmethodexistsforaccountingfortheeffectofReynoldsnumber.Thiswillbediscussedinmoredetailsinchapter12.2.
-
7/23/2019 Experimental Methods in Marine Dynamics
12/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page11
AssumingFroudescalingisappliedandgeometricalsimilaritywithscaleratio /F ML L ,
fromtheequalityinFroudenumberwehave:
M F
M F
FF M M
M
U U
gL gL
LU U U
L
Theotherphysicalparameterscannowbederivedfromthedimensionalanalysissfollows:
Structuralmass:3F
F M
M
M M
Force:
3F
F MM
F F
Moment: MM
F
F MM4
Acceleration: F Ma a
Time: F Mt t
Pressure: FF MM
p p
Theratio F M isincludedtoaccountforpossibledifferenceinfluiddensitybetweenfullscale
andmodelscale(usuallyseawaterinfullscalerelativetofreshwaterinthetesttank).
2.5 Hydroelasticity
Inhydroelasticproblemsthehydrodynamicforcesareinfluencedbytheelasticdeformationofthe
structure.Thisdeformationisgovernedbytheinertiaforcesandelasticforcesinthestructure.Themodellingoftheelasticpropertiesofstructureswillthereforegiveseveraladditionalproblems
comparedtothemodellingofwaveinduceddynamicresponseofrigidstructures.Exampleswhere
correctlyscaledelasticbehaviourofthemodelwillbeimportantisspringingandwhippingofships,
anddynamicbehaviourofmarinerisersandmooringlines.
Additionalrequirementstotheelasticmodelcanbesummarisedasfollows:
Correctlyscaledglobalstructuralstiffness
Structuraldampingmustbesimilartofullscalevalues
Themassdistributionmustbesimilar.
-
7/23/2019 Experimental Methods in Marine Dynamics
13/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page12
Geometricalsimilaritybetweenmodelandfullscaleforanelasticstructurewillrequirethat
theelasticdeformationsaresimilar.Toillustratethiswewillconsiderthedeflectionofacantilever
beamasanexample.Thedeflection,,isgivenfrom:
EI
FL3
whereEIistheflexuralrigidityandFisthehydrodynamicforcewhichcanbeexpressedas:
22LUCF
whereCisaforcecoefficientdependentonFN,Reetc.Therequirementofsimilarityindeformation
inmodelandfullscalegives:
F MF M
F ML L
Usingtheaboveequationsthisrequirementissatisfiediftheratio:
2 4C U L
EI
isequalinmodelandfullscale.Assumingequalforcecoefficientanddensityweobtainthe
followingrequirementtothestructuralrigidity:
2 4 2 4
5
F M
F M
U L U LEI EI
EI EI
Ifalldimensionsofthecrosssectionalshapeofthebeamarescaledgeometricalsimilar,the
momentofinertia,I,willsatisfytherelation:
4
F MI I
WearethanleftthefollowingrequirementtotheYoungsmodulus,E:
F ME E
ThisimpliesthattheYoungsmodulusforthemodelmustbe1/timesthevalueofthefullscale
structure.
Itshouldbenotedthatthetwolastequationsisnottoberegardedasrequirementstothemodel.
ThebendingstiffnessrequirementisgivenforEI.Inpracticalmodeltestingtherequirementgiven
toscalingofEIisoftensatisfiedbymanipulatingthedifferentparametersbyapplyingother
materials,otherwallthickness,orbymodifyingthestructuralbuildupofthebeam.Theouter
geometry,whichisexposedtothehydrodynamicforces,hastobemodeledgeometricallycorrect.
Alsotherequirementtocorrectmodelingofmassdistributionandstructuraldampinghastobe
satisfied.Thiswillbefurtherdiscussedaspartofthephysicalmodeling,seechapter5.3.
Similarresultswillbefoundfortheaxialandtorsionstiffnesses.Therequirementfortheaxial
stiffnesscaseis:
-
7/23/2019 Experimental Methods in Marine Dynamics
14/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page13
3)()( MF EAEA
whereEAistheaxialstiffness.Thisrelationgivesequalstraininmodelandfullscale.Thecross
sectionalarea,A,willsatisfytherelation2
MF AA ,whichgivesthesamerequirementtothe
Youngsmodulusasshownabove.
2.6 Cavitation
Ifcavitationoccurs,dynamicsimilarityalsorequiresthatthelawofequalcavitationnumberis
accountedforintheexperiments.Therequirementisthatthecavitationnumbergivenas:
0
2
( )
1/ 2
vgh p p
U
hastobethesameforthemodelasinfullscale.p0istheatmosphericpressure,ghisthe
hydrostaticpressureandpvisthevapourpressure.Tosatisfythisrequirementacavitationtunnel,
withpossibilitytolowertheatmosphericpressurehastobeapplied.
-
7/23/2019 Experimental Methods in Marine Dynamics
15/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page14
3 EXPERIMENTALFACILITIES
3.1 Introduction
Thedifferenttypeofexperimentalfacilitiesusedforshipsandoffshorestructurescanbe
categorizedasfollows:
Towingtanks,conventionalandfacilitiestailormadeforspecificpurposes.
Cavitationtunnels
Oceanbasins
Usuallywewillfindtwoormoredifferenttypeoftestsfacilitiesateachresearchandtesting
institution.ForexampleatMARINTEKthereisthreetowingtanks,acavitationtunnelandanocean
basin.InFigure3.1anoverviewofthetestfacilitiesatMARINTEKispresented.
Theexperimentalfacilitiesfortestingofshipandoffshorestructuresarenotonlythephysicaltank/basinwherethetestsareexecuted.Thetestingfacilitieshavealsotocoverdifferent
additionalfunctionsasworkshopsforconstructionandbuildingofmodels,instrumentation,
simulationofenvironmentandsoftwareandtoolstorecordandanalyzethemeasureddata.A
typicallayoutofatowingtank,includingutilityfunctions,isshowninFigure3.2. Fortestingof
realisticbehaviorofstructuresinaseaway,equipmentforgenerationofwind,wavesandcurrent
andefficientwaveabsorptionareofvitalimportance.
3.2 Towing
Tanks
Thefirsttowingtankswerebuiltforperformingtowingandpropulsiontests.Thelengthofthe
towingtankhastobelongenoughtogetasufficientlongtimewithsteadyflowconditionsfor
measurementsoftowingandpropulsionforces.Therequiredsizewillthereforebedependenton
typeofshipstobetested,scaleratioandforwardspeed. Todayalargenumberoftowingtanks
exist,morethan200areinregularuse. Thelengthofthetowingtanksisfrom20mtomorethan
1000m.
Thesmalltanksaretypicallyconnectedtoteachingandresearchinstitutions.Theverylongtanks
aremainlyconnectedtonavalactivities.AnexampleisthehighspeedtankatDavidTaylorNaval
ShipResearchandDevelopmentCentrewithdimensions900mx6.4mx3mwithamaximum
towingcarriagespeedofupto50m/s.Thistankwasbuiltespeciallyfortestingofhighspeedships.
Theconstructionofthistankwasadirectresultoftherequirements:Navyin50kn,definedin
about1960asatargetfortheUSNavy.AsimilarfacilityalsoexistsinSt.Petersburg.
AtypicalsizeforcommercialworkingtowingtanksisLxBxd=250mx10mx5m. Typicalshipmodel
lengthis58m.Thissizeoffacilitiesseemstorepresentareasonablecompromisebetweencostfor
tankconstruction,costformodelmanufactureandoperationalcosts(whichtogetherdetermine
thecostofmodeltesting)andtherequiredscaleratioandcorrespondingaccuracythatcanbe
achieved.ThesizeofthelargehydrodynamiclaboratoriesattheMarineTechnologyCentreis
showninFigure3.1,withmoredetailsaboutthetowingtanksgiveninFigure3.3.
-
7/23/2019 Experimental Methods in Marine Dynamics
16/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page15
Almostalltowingtanksuseatowingcarriagetomovethemodeltroughthewater.A
typicaltowingcarriagedesignisshowninFigure3.3.Thetypicalmaxcarriagespeedis10m/s.
Duringcalmwatertowingandpropulsionthemodeliskeptfixedinsurgeswayandyaw,butfreeto
heaveandpitch.
Figure 3.1 Overview of test facilities at MARINTEK
-
7/23/2019 Experimental Methods in Marine Dynamics
17/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page16
Figure 3.2 A typical towing carriage design.
Tobeabletoperformseakeepingtestsorothertypeoftestinginsurfacewaves,manytowing
tanksareequippedwithawavemakeratoneendofthetank.Generationofwavesandtypeofwavegeneratorsarediscussedinmoredetailsinchapter3.5.1.Inordertopreventreflectionsof
wavesfromtheoppositeside,awavebeach,whichisabsorbingthewaveenergy,hastobe
installedatthissideofthetowingtank.
Ithasalsobeenconstructedtowingtanksthatarehighlyspecialisedforagivenpurpose.An
exampleistheDutchandChinesevacuumtanks,wheretheentirespaceabovethetankis
evacuatedandairpressuredownto0.04barcanbeachieved.Thepurposeofthistypeoffacilityis
todopropulsiontestswithsurfaceeffectsandcompleteshipmodelpresent,atthelowpressure
requiredforequalityincavitationnumber.
AnotherexampleofaspecialisedtankistheicetanksinHamburgandHelsinki.Iceismodelledby
freezing,usinghighsalinitywaterandchemicalstocontrolthemechanicalprioritiesoftheice.
Thesetanksareusedfortestingoficebreakersandoffshorestructuresexposedtotheactionof
driftingice.
ThetowingtankatMARINTEKwascompletedin1939withdimensions170x10.5x5m.Later,in
1978,extendedto260mwherethedepthoftheextensionis10.0m.Thelayoutofthetowingtank
isshowninFigure3.4.Thetowingcarriageisofconventionaltype. Fortestingofhighspeed
vesselsthecarriageisequippedwithaFreetoSurgerig.The8mlongrigismountedinfrontof
thetowingcarriageasshowninFigure3.4.Usingthisrigthewinddisturbanceatthepositionofthe
modeliseliminatedandthemodelisallowedtofreelysurge,heaveandpitchduringwavetesting.
-
7/23/2019 Experimental Methods in Marine Dynamics
18/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page17
Towingtankdata
TankI TankII TankIII TankI+III*
Length:
Width:
Depth:
175m
10.5m
5.6m
25m
2.8m
1.0m
85m
10.5m
10m
260m
10.5m
5.6/10.0m
Tot.weightcarriage:
Wheelbase:
Speedrange:
Max.acceleration:
20tons
11.04m
0.0210m/s
1m/s2
0.2ton
3m
0.051.75m/s
1m/s2
15tons
11.04m
00.9m/s
1m/s2
20/15tons
11.04m
0.0210m/s
1m/s2
Modelsizerange: 8m 1m 8m
Wavemaker:
Max.waveheight:
Waveperiodrange:
Max.wavesteepness:
Singleflap
Regularandirregularwaves
0.3m
0.253sec.
1:8
Doubleflap
Regularandirregularwaves
0.9m
0.85sec.
1:10
Doubleflap
Regularandirregularwaves
0.9m
0.85sec.
1:10
Wavespectra: Computergenerated
* Tank I and III can be used separately and also as one long tank (Tank I + III) by removing the gate (12)
and wave absorber (15). In Tank I + III either of the two carriages can be used.
Figure 3.3 Towing Tanks at MARINTEK.
11
4
10 9 8 7
136
5
3 2 1
1
5.
6
10.
0
28
39 85
260
13.
5
10.
5
Model store
Drawing office
Reception
TankII
Ship model manufacturing
shop
Trimming tank
NC milling machine for
model production
Instrumentation workshop
Carpenter workshop
Propeller model
manufacturing shop
Cavitation laboratory
Dock gate
Wave absorber, Tank I
and Tank I+III
Wavemaker, Tank III
and Tank I+III
Wave absorber, Tank III
12 15
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
TANKI TANKIII 1
-
7/23/2019 Experimental Methods in Marine Dynamics
19/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page18
Figure 3.4 Free to surge rig in front of towing carriage.
3.3 CavitationTunnel
Cavitationtunnelsaredesignedtobeabletotestpropellersandotherliftingsurfacesata
sufficientlylowpressuretoachievecorrectcavitationnumber.Mostcommercialmodeltest
institutionshaveoneormorecavitationtunnels,andabout100tunnelsistodayinregularuse.
Awiderangeofdifferentsizecavitationtunnelsexist,fromsmallsizetunnelsforresearchand
education,with
test
section
area
of
typically
0.25
x0.25
m,
to
very
big
circulating
water
tanks,
with
testsectiondimensionupto3x6mandlengthof11m(theBerlintunnel).Atypicalsize
conventionaltunneliswithcirculartestsectionwithdiameterofabout1mMaximumflowspeed
atmeasuringsectionisusually1020m/s.Largetunnelsoftenhavetestsectionsallowingfor
mountingofacompleteshiphullmodel.
Fortunnelsthatcannotallowtestingofentireshiphullmodels,anafterbodymodeloftheshipis
oftenappliedtoproducecorrectinflowtothepropeller,andmeshscreensareusedtoproducethe
specifiedwakedistribution.Thebenefitofusingafterbodymodelsandmeshscreens,insteadofa
completemodel,isthepossibilityofhavingthemeshscreensimulatefullscalewake,notonly
modelscalewake.Whentestingtheentireshipmodel,onlymodelscalewakemightbetested.
Somecavitationtunnelsareofthefreesurfacetype.Suchtunnelscanbeusedfortestingofhigh
speedpropellersoperatinginfullorsubmergedcondition.Thistypeoftunnelsisespeciallywell
suitedforstudyingventilationproblemsforpropeller,waterjetsandfoilsections.Largetunnels
withfreesurfaceenabletestwithnormalshipmodels.
ThecavitationtunnelatMARINTEKisshowninFigure3.6.Thediameteroftheworkingsectionis
1.2mandthelengthofworkingsectionis2.08m.Maximumwatervelocityis18m/s.The
minimumworkingpressureis0.1atm.Afterbodymodelsandmeshscreensareapplied.
-
7/23/2019 Experimental Methods in Marine Dynamics
20/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page19
Figure 3.5 Cavitation Tunnel at MARINTEK.
-
7/23/2019 Experimental Methods in Marine Dynamics
21/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page20
3.4 OceanLaboratories
Theoceanlaboratoriesareingeneralconstructedfortestingofoffshorestructuresandfor
seakeepingandmanoeuvringtestingofships.
Incontrasttothetraditionaltowingtankstheoceanbasinsandseakeepinglaboratoriesmakeit
possibleto
carry
out
tests
with
any
wave
heading
(oblique
waves)
for
ships
with
forward
speed.
For
manoeuvringtestsitisrequiredwithatowingcarriagewithcontrolledmotionsinbothlongitudinal
andtransversedirection.Thisisachievedbyasubcarriage,whichisconnectedunderneaththe
mainlongitudinalmotioncarriage(seeFigure3.7,takenfromtheseakeepinglaboratoryatSSPA,
Sweden).Combinedwiththelargewidthofthesefacilities(typically3050m)thearbitrary
horizontalmotionrequirementtendstomakethecarriagesystemcomplexandheavy.
Basinspurposebuiltforoffshoretestingisformostcasesbuiltafter1980.Foroffshoretestinga
largecarriagesystemisnotrequired.Oceanlaboratoriesareusuallyequippedwithadvanced
systemsforgenerationofwaves,oftencapableofgenerationofbothlongcrestedand
multidirectional(or
short
crested)
waves
as
well
as
wind
and
current.
In
this
way
it
is
possible
to
givearealisticrepresentationofthemarineenvironmentalconditions.
Figure 3.6 Carriage system in Ocean Basin (from SSPA, Sweden).
Examplesofcommercialoceanlaboratoriesfortestingofcoastalandoffshorestructuresare:
MARINTEK,Trondheim; LxB=80mx50m,d=010m
MARIN,Netherlands; LxB=45mx36m,d=010.5m,pitincentrewithd=30m
HydralicLab,Ottawa,Canada: LxB=50mx30m,d=3m
OTRC,TexasA&M: LxB=45.7mx30.5m,d=5.8m,pitwithd=16.8m
-
7/23/2019 Experimental Methods in Marine Dynamics
22/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page21
Somebasinsareequippedwithafalsebottomthatcanbesettodifferentdepths.Inthis
waytheactualwaterdepthcanbecorrectlymodeledinthetestsetup.Thispropertyalsoenable
mountingofmodels,mooringsystemandothersubseaequipmentonadrybottom,whichafter
installationofthesystemtobetested,islowereddowntothewantedwaterdepth.Thislargely
simplifiesthepreparationworkforthetest.
TheoceanlaboratoryatMARINTEKisfittedwithtwosetsofwavemakers.Alongthe50msideof
thebasinthereisadoubleflapwavemakercapableofgeneratinglongcrestedwaves.Alongthe80
msidethereisamultiflapwavemakerconsistingof144individuallycontrolledflapsforgeneration
ofshortcrestedandlongcrestedwaves.Waveabsorptionbeachesareinstalledonthetwo
oppositesidestoreducetheproblemswithwavereflections.Currentcanbemodeledindirection
alongthebasin(inwavedirectionofthedoubleflapwavemaker).Thewaterdepthisadjustable
from0m(surfaceposition)to10mbymovingthefalsebottom.Amoredetaileddescriptionofthe
OceanLaboratoryatMARINTEKisgivenbyHuseandTrum (1981)andNaeser.(1981).
3.5 Generationofenvironment
Reliablemodeltestingrequirescontrolledgenerationofwind,wavesandcurrentinbothtimeand
spacetoachievearealisticandwelldefinedenvironment.Commonlyusedequipmentfor
environmentgenerationisdescribedinthefollowing.
3.5.1 Wavegenerationandabsorption
Therearetwomainclassesofwavegenerators,thehorizontaldrivenflaptypewavemakerandthe
verticaldrivenwedge(plunger)typewavemaker.Inmoderntestfacilitiesalmostonlytheflaptype
isused.TwoexamplesofflaptypewavemakersareshowninFig3.8.Thefirstoneisadoubleflap
wavemakerasinstalledinthetowingtankandintheoceanbasinatMARINTEK.Hydraulic
actuatorsareused.TheotheristhesingleflapwavemakerasinstalledinMarineCybernetic
Laboratory(MCLab)atMARINTEK.Thiswavemakeriselectricallydriven.Therearsideoftheflap
maybeeitherdryorwet. Thedoubleflaptypeisusuallyusedfordeeperwater.Bythepossibility
ofusingtheupper,thelowerorbothflapsincombinationsforthedoubleflaptype,itispossibleto
generatewaveswithaminimumofdistortionforlargerwavelengthrangethanwhatispossiblefor
asingleflapsolution.
-
7/23/2019 Experimental Methods in Marine Dynamics
23/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page22
Figure 3.7 Examples of flap type wave maker; single flap and double flap.
Othertypesofwavemakersarepistontype(asmallsketchisshowninFigure3.9),andpneumatic
wavemakers.Pneumaticwavemakersusevariableairpressureinachamberabovethewaterat
theedgeofthebasintocreatewaves.DavidTaylorModelBasininWashingtonDChasapneumatic
wavemakerintheiroceanbasin,exceptforthattheprincipleislittleused,andisconsidered
inferiorrelativetoflaptypewavemakers.
Figure 3.8 Wave-maker theory, Wave height to stroke ratio as function of relative depth.
-
7/23/2019 Experimental Methods in Marine Dynamics
24/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page23
Thegenerationofwavesarecontrolledbythefrequencyandamplitudeoftheflap.In
Figure3.9therelationbetweenflapstroke,S,andwaveheightH,isshownforflaptypewave
maker.Theresultingwaveheightisshownasafunctionoftheparameterkhwhere 2k is
thewavenumber,isthewavelengthandhisthewaterdepth.Theresultsarebasedonwave
makertheoryseee.g.DeanandDalrymple(1984).Thisratiobetweenthemechanicaldisplacement
ofthe
flap
to
the
wave
amplitude
is
the
transfer
function
of
the
wave
maker.
Aregularwaveelevationcanbegeneratedusingthetransferfunctiontodeterminetherequired
controlsignaltothewavemaker.InFigure3.10themaximumwaveheightforregularwavesas
functionofwaveperiodisshownforthedoubleflapwavemakersinthetowingtankatMARINTEK.
Itisobservedthatincreasingwaveperiod(andhencewavelength),givesdecreasingmaximum
waveheight.
Figure 3.9 Maximum wave height as function of wave period, Double Flap wave maker at
MARINTEK
Thegenerationofirregularwavesiscontrolledbyaninputsignalbasedontheselectedwave
spectrum
combined
with
the
transfer
function
of
the
wave
maker.
The
commonly
used
assumption
thattheseasurfaceelevationisastationaryGaussianprocesswithzeromeanisapplied. The
surfaceelevationasfunctionoftime,(t),canthanberepresentedbyafinitenumberofFourier
components:
1
( ) cos( )N
n n n
n
t a t
wheren isthephaseangleofcomponentncreatedfromarandomphasegenerator.Random
phaseisnecessarytoeliminateanycoherentfeaturesdevelopinginthewavesignal.anisthe
FourieramplitudeofcomponentndeterminedfromtheinputwavespectrumdensityS()as:
2 ( )n na S
-
7/23/2019 Experimental Methods in Marine Dynamics
25/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page24
isthefrequencyintervalforeachcomponent.Itisimportantwithasufficientnumberof
componentsinthewavegenerationtoavoidrepetitionofthewavesignalandaliasing,see
Newland(1975)forfurtherdetails.Typically,2000componentsareused.
FormostcasesthewavespectraaregeneratedaccordingtotheJONSWAPformulation:
2020 2()(exp4
052 )(25.1exp)( gS
where:
07.0 for 0
09.0 for 0
0 isthespectralpeakfrequency
isthepeakednessparameter.
InFigure3.11atypicalexampleoftheoreticalJONSWAPspectrumandmeasuredwavespectruminthewavetankareshown.Theagreementinenergydistributionisseentobeverygood.
Figure 3.10 Typical example of theoretical JONSWAP spectrum and measured wave spectrum in
the wave tankMultidirectional(orshortcrested)wavescanbegeneratedusinganarrayofflapsalongonesideof
thebasin.Therearetypicallyaboutahundredindividualflaps.Themultiflapwavegeneratorscan
-
7/23/2019 Experimental Methods in Marine Dynamics
26/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page25
alsobeusedtogeneratelongcrestedwaveswithanarbitrarywaveheading. Togenerate
shortcrestedwavethedirectionalspreadingfunctionmustbespecifiedinadditiontotheenergy
densityspectrum.Thisgivesthefollowinggeneralisationforthesurfaceelevationasfunctionof
spaceandtime,(x,y,t):
nnnnnN
n
n tyxkatyx )sincos(cos),,( 1
whereannowistheFourieramplitudeofcomponentnincludingthespreadingfunction:
),()(2nnnn DSa
Toavoidreflectionandwavebuildingupinthebasin,anefficientwaveabsorptionsystemisalso
essential.Themostusedsystemforwaveabsorptioniswavebeaches.Anexampleisshownin
Figure3.12.Theshapeisparabolicwhichhasbeenfoundtobemoreefficientforalargewave
periodrangecomparedtoastraightbeach. Reflectedwaveheightoflessthan5%oftheincoming
waveheightwilltypicallybeachievedwiththisbeachdesign. Inoceanbasinswaveabsorbersareusuallymountedonthesideswithoutwavemakers,typicallywithtwosideswithwavemakersand
twosideswithwaveabsorbers(asinMARINTEKoceanbasin).
Intowingtanksthemainproblemwillbereflectionoftheshipgeneratedwavesystemfromthe
tankwalls.Itisnotpracticaltomountabeachalongsidethetankwallandtransversewaveswillbe
generated.Fortestswithforwardspeedthisisusuallynotaproblem,sincethereflectedwaveswill
hitthetestareaafterthemodelhasleft.Fortestswithzeroorverylowforwardspeed,the
problemofwavereflectionsmustbetakenveryseriously.Forlongtestruns,likeistypicalforatest
inirregularwaves,somekindofwaveabsorptionalongthetankwallisrequired.
-
7/23/2019 Experimental Methods in Marine Dynamics
27/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page26
Figure 3.11 Upper; Wave absorber, beach type. Lower; measured wave reflection from beach, in
% of incoming wave amplitude.
3.5.2 Windgeneration
Windgenerationismostconnectedtostationarymodeltestsinoceanbasins.Forfreelymoving
modelswind
is
not
easily
applied
in
practical
testing.
The
wind
in
the
basin
is
usually
generated
by
meansofabatteryofportableelectricalfans.Thefansareplacedsomedistancefromthetesting
areatoachieveahomogeneouswindspeeddistributionatthepositionofthetestmodel.Thewind
directioncanbechangedbymovingthepositionofthefans.
Twodifferentmethodsforcalibratingthewindspeedarecommonlyused:
1. Froudescalingofwindspeed,i.e: WindFWindM UU ,,
2. Usingprecalculatedwindforceactingonthemodelandtuningthemodelwindspeedto
thisforce
is
achieved.
Forthefirstcasethewindspeediscalibratedatthepositionofthemodel,butwithoutthemodel
present.Usingthisprocedurerequireaveryaccuratemodellingofthemodelsuperstructureto
obtainreliablewindforces. Thelastprocedurerequiresthatreliablewindforceestimatesare
availableonbeforehand.Ifthisisthecasethescaleeffectsonwindforcescanbeavoided.Usually
thisprocedurewillgiveabout20%higherwindspeedthanthespeedestablishedfromFroude
scalinglaw.
Theeffectofwindwillbeimportantforalmostalltypesofmooredstructures.Thewindspeedisin
general
non
steady
and
the
dynamic
effects
of
the
winds
can
be
an
important
exaction
source
for
resonancemotionsofmooredstructureandinspecialcasesforrollmotionsofships.Thedynamic
-
7/23/2019 Experimental Methods in Marine Dynamics
28/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page27
effectofwindcanbesimulatedinthetestbycontrollingthepowertothefans.A
frequentlyusedwindenergyspectrumforoffshoreapplicationsistheNPDspectrum.
Thefrequencyrangeofawindspectrumisquitebroadbanded,oftencoveringarangefrom0.005
to1Hz.
3.5.3
Current
Tosimulatecurrenttwodifferentapproachesarecommonlyused:
1. Directgenerationofcurrentinthebasinusingpumpingofwater
2. Towingofthemodelsetupwithspeedequaltothecurrentspeed.
Thefirstapproachrequireslargepumpswithrecirculationducts.Forbasinswithafalsebottom(as
atMARINTEK)thepumpscanrecirculatethewaterunderthefalsebottom. Alsoexternalpiping
(outsidethebasin,asusedinMCLabatMARINTEKandatMarinintheNetherlands)canbeusedfor
recirculationofwater.
Localcurrentcanbegeneratedbyplacingportablecurrentgeneratorsinfrontofthemodel(in
principleasforthewindgeneration).Howeverforthismethoditisdifficulttoachieveareasonable
stationarycurrentfieldatthepositionofthemodelduetolargeeddiesofbackflowingwater.The
effectofcurrentonwaveforceswillnotberealisticallyaccountedforbythisproceduredueto
largespacevariationincurrentfieldbetweenthewavemakerandmodel.
Theeffectofcurrentisespeciallyimportantformooredstructures,bothduetothedirectforces
duetothecurrentandduetotheinteractionbetweencurrentandwaves.Theinteractionbetween
currentandwaveseffectcanlargelyinfluencethewavedriftforcesandhenceinfluencemean
offsetandforcesaswellastheslowdriftmotions.Forthecasewithmooredstructuresthe
simulationofthecurrenteffectbytowingthemodelwithaspeedequaltothecurrentspeedisnot
apracticalsolution.Forthiscaseabasinwithdirectcurrentgenerationwillberequired.
ThegenerationofcurrentspeedisbasedontheFroudescalinglaw.Thisisnecessarytoproperly
representthewavecurrentinteractioneffects,butitmayintroducesomescaleeffectsforthe
currentforcesduetodifferenceinRenumber,resultinginpossiblydifferentflowregimesinmodel
andfullscale.
Currentcalibrationofspeedandprofileshouldbeperformedwithoutthemodelinthebasin.
Velocityfluctuationswillalwaysbepresentinbasingeneratedcurrent(inrealfullscalecurrent,
fluctuationswillalsobeobserved).Largefluctuationsincurrentmayrepresentanexcitationsource
forslowlyvaryingresonanceoscillationsandthemagnitudeshouldthereforebeaslowaspossible.
Astandarddeviationforthecurrentfluctuationofabout5%ofmeancurrentistypicallyachievedin
basinswithclosedrecirculationsolutions.Correctmodellingofthecurrentfluctuationsmightbe
importantforthedynamicsofdeepwatersystems,butwestillnotknowenoughaboutthis,andno
modeltestingfacilitiescurrentlyhavepossibilitiestocreatecontrolledcurrentfluctuations.
-
7/23/2019 Experimental Methods in Marine Dynamics
29/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page28
4 INSTRUMENTATION
4.1 Generaldescriptionofequipment
Alargerangeofdifferenttypeofmeasuringequipmentisusedfortestingofshipsandoffshore
structures.Usually,instrumentsaredesignedtogenerateananalogvoltageorcurrentsignalwhich
islinearlyproportionaltothemeasuredparameter.Nonlinearcharacteristicsoccurinrarecases.
Instrumentswithdigitaloutputareincreasinglyused,butanalogoutputisstillpreferred,inorder
toavoidthecomplexitiesofdealingwithdifferentdigitalsignalprotocols.
Thesystemrequiredforperformingmeasurementsincludesthefollowingcomponents:
Thetransducers
Amplifiers
Filters(analogand/ordigital)
ADconverter
Datastorageunit
Cablingbetweenthedifferentcomponents
AtypicalsetupisshowninFigure4.1.Itiscommonpracticetousetwoormoreindependent
computersystemsforoperatingthetankfacility.Onemachineisusedforrealtimegenerationof
controlsignalforthewavemakerandanadditionalmachineisusedforthedataacquisitionand
analysis. Additionalmachinesmightbeusedforcontrolofruddersorothercontroldevices,orfor
controlofthecarriage.
Figure 4.1 Schematic of typical set op of a data acquisition system for model testing
Afurtherdescriptionofinstrumentationandtransducersrelevantformodeltestingcanbefoundin
Olsen(1992).Adetaileddescriptionofmeasurementtechniquesforfluidmeasurementsisgivenby
Goldstein(1983)
4.2 Strainanddisplacementmeasurements
Themostusedmethodsforstrainanddisplacementmeasurementsinmodeltestingarebasedon
thefollowingprinciples:
Resistivetransducers, basedonchangeofresistanceduetostrain; straingauges
Inductivetransducers Capacitancetransducers.
TRANSDUCER
AMPLIFIER& SIGNALCONDITIONER
A/DCONVERTER
RESPONSE
C
OMPUTER
DATABUS
-
7/23/2019 Experimental Methods in Marine Dynamics
30/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page29
Inadditiontoadirectmeasureofstrainanddisplacements,thesetypeoftransducerare
alsocommonlyusedasthebasisforpressurecells,forcetransducers,velocitymeasurementsand
accelerometers.Theseapplicationswillbediscussedseparately.
4.2.1 Straingauges
Thestrain
gauge
measured
the
elongation
in
the
material
to
which
it
is
glued.
Strain
gauges
are
commonlyusedinanumberofdifferenttypesoftransducers.Examplesofstraingauge
constructionsareshowninFigure4.2.ThethreadsareusuallyCUNialloys.
Theuseofstraingaugesisbasedonthattheelongationofthestraingaugewillchangethe
resistance.Thegaugefactork,isdefinedas:
LL
RR
k
whereR
is
the
resistance
and
Lis
the
length
and
represent
the
change
of
length
or
resistance.
The
factork istypicallyabout2formetallicmaterials.Increasingthefactorkwillincreasethe
sensitivityofthestraingauge. kvaluesuptoabout100200canbeachievedusingpiezoresistive
materials.
Theelongationofthestraingaugesususuallymeasuredinmicrostrain,S=106S,where
LLS .
Figure 4.2 Examples of strain gauges designs
Tomeasure
the
change
of
resistance
over
astrain
gauge,
a
Wheatstonebridgecircuitisused.AbasicWheatstone
bridgecircuitcontainsfourresistances,aconstantvoltage
input,andavoltagegage.ForagivenvoltageinputVin,the
currentsflowingthroughABCandADCdependonthe
resistances,i.e.,
4321 RRIRRI
VVV
ADCABC
ADCABCin
Thevoltage
drops
from
A
to
B
and
from
A
to
D
are
given
by:
Figure 4.3 Wheatstone bridge circuit
-
7/23/2019 Experimental Methods in Marine Dynamics
31/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page30
4
34
4
1
21
1
RRR
VRIV
RRR
VRIV
in
ADCAD
in
ABCAB
ThevoltagegagereadingVgcanthenbeobtainedfrom:
in
inin
ADABg
VRRRR
RRRR
RRR
VR
RR
VVVV
3421
4231
4
34
1
21
Nowsupposethatallresistancescanchangeduringthemeasurement.Thecorrespondingchange
involtagereadingwillbe:
ingg
VRRRRRRRRRRRRRRRRVV
33442211
44223311
Ifthebridgeisinitiallybalanced,theinitialvoltagereadingVgshouldbezero.Thisyieldsthe
followingrelationshipbetweenthefourresistances:
rR
R
R
RorRRRR
VRRRR
RRRRV ing
1
0
3
4
2
14231
3421
4231
Wecanusethisresulttosimplifythepreviousequationthatincludesthechangesinthe
resistances.DoingsoresultsinthesolutionforthechangeinVg:
ing VR
R
R
R
R
R
R
R
r
rV
1
1 4
4
3
3
2
2
1
1
2
whereisdefinedby:
3
3
2
2
4
4
1
1
1
1
1
R
R
R
Rr
R
R
R
R
r
Moreover,whentheresistancechangesaresmall(
-
7/23/2019 Experimental Methods in Marine Dynamics
32/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page31
Inpractice,oneoftenusesthesameresistancevalueforallfourresistors,R1=R2=R3=R4=R.
Notingthatr=1inthiscase,thechangeinvoltagecanbefurthersimplifiedto
ing VR
RRRRV
4
4321
DifferenttypesofWheatstonebridgecircuitsareusedtomeasurethechangeofresistanceoverastraingauge. Averysimpleexampleformeasurementofforceisshowninfigure4.4. Onestrain
gaugeismountedtoeachsideofabeam.Twodummyresistances(usuallyintegratedinthe
amplifier)areusedforbalancingthebridge. Thissetupiscalledahalfbridge.Aconstantvoltageis
usedasexcitation,Vin.Theforcegivesrisetoanelongationofstraingauge1andcompressionof
straingauge2.Thisintroducesanunbalanceinthebridgeandavoltagecanbemeasuredatthe
exitatVg.Inafullbridgecircuit,allfourbranchesofthebridgearestraingauges.Mountingtwo
straingaugesoneachsideofthebeaminFigure4.4inafullbridgearrangementwouldgivetwice
thesensitivityofthehalfbridgearrangement.
Figure 4.4 Examples of half-bridge circuit for measurements of change of resistance of strain
gauges.
4.2.2 Inductivetransducers
Theinductivetransducersarebasedonthevoltageinducedbyamovablecore.Anexampleofan
applicationisshowninFigure4.5.TheshownsystemiscalledLVDT(linearvariabledifferential
transformer).OnesetofthecoilisexcitedbyACvoltageandtheinducedvoltageismeasuredin
thesecondset.
Thistypeoftransducerisavailableinawiderangeofsizes,frequencyrangesandaccuracys.Itis
usedfordirectpositionmeasurements,butalsoasbasisforpressurecellsforcetransducers,
velocitymeasurementsandaccelerometers.
1 2
Side view Front view
Force K
Straingauges R
+R
R
R-
R
R
A B
B
C
VgG
Vin
-
7/23/2019 Experimental Methods in Marine Dynamics
33/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page32
Figure 4.5 LVDT transducer for displacement measurements.
4.2.3 Capacitancetransducers
Thecapacitancetransducersconsistoftwocloselyspacedplatesoraplatesuspendedbetweena
pairofouterplatesasshowninFigure4.6.Theplatesareconductiveandrelativemovement
betweentheplatesintroduceavariationofthecapacitance
Figure 4.6 Capacitance transducers for displacement measurements.
Thistypeoftransducersrequireamuchsmallerdrivingforcecomparedtoinductivetransducers,
buthaveahighernoiselevelandarethereforelessfrequentlyusedinpracticalmodeltesting.
4.3 Positionmeasurements
Typicalpositionmeasurementsofinterestforfloatingstructureswillbethe6degreesoffreedoms
rigidbodymotionsofship/platformsandmotionsofmooringlinesandrisers. Otherexamplesare
measurementsofdeflectionsofelasticmodelsasforspringingandwhippingresponseofships.
4.3.1 OpticalandVideosystems
Forfreerunningmodelsandmooredstructurestheglobalmotionsaremeasuredbyopticalor
videobasedsystems.Foropticalsystemminimum3lightemittingdiodesarelocatedonthemodel.
F
F
-
7/23/2019 Experimental Methods in Marine Dynamics
34/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page33
Forvideosystemsballshapedreflectorsmountedonthemodelisused.Onshorecameras,
minimum2,areusedforreadingthepositionofeachdiode.Basedontheinstantaneousposition
(x,yandz)ofeachofthe3diodes,themotionsin6DoFaredetermined.
Theaccuracyofthemeasuredmotionswillforbothopticalandvideosystemsbeoftheorderof
+/ 1mmforposition(inmodelscale)and+/0.05degreesforroll,pitchandyaw.Formostcases
thisisanacceptableaccuracyfortherigidbodyvesselmotions.
4.3.2 Gyros
Therollandpitchmotionscanalsobemeasuredusinggyros. Theprinciplebehindthegyrois
showninFigure4.7.Arotatingmasskeepstheinnerpartofthegyroinacontinuoushorizontal
position.Thenextlinkcanbetiltedaboutoneaxisandtheangleismeasuredusinga
potentiometer. Theouterlinkcanbetiltedaboutanaxisperpendiculartothefirstaxisandthe
anglecanbemeasuredinthesameway. Fromthemeasuredanglesandtheknownsequenceof
theanglestherollandpitchmotionsareuniquelydetermined.
Thegyroisarobusttoolandiscommonlyusedbothinmodeltestingandininstrumentsappliedin
fullscale.However,sinceitinvolvescomplexmechanicalcomponents,itisfairlylargeandfairly
expensive.Thesizelimitstheuseinmodels,andthecostlimitstheusebothinmodelandinfull
scaleexperiments.
Figure 4.7 Principle of a gyro for measurement of roll and pitch.
4.3.3 Potentiometer
Lowfrictionpotentiometerscanbeusedformeasurementofmotioninonedirection.ANylonline
isconnectedtothemodel,thenpassedaroundthepulleyonthepotentiometerspindleand
tensionedbysprings.Themotionofthemodelwillthereforebedirectlytransducedintoavoltage
signalbythepotentiometer.
Acommonlyusedsetupformeasurementsofheaveandpitch(trim)fortowingtestsisshownin
Figure4.8. Thepotentiometersareusedformeasurementsofthemotionsbetweentheshipmodelandthetowingcarriage.Thesetupisusedbothformeasurementsofrunningheaveandtrimin
calmwatertestingandformeasurementsofwaveinducedmotionsinheadseawaves.
-
7/23/2019 Experimental Methods in Marine Dynamics
35/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page34
Figure 4.8 Example of using potentiometers for measurements of heave and pitch motions in
towing tests.
4.3.4 Positionbasedonmeasuredforceandacceleration.
Measurementofpositioncaninprinciplebeobtainedfrommeasuredacceleration(seebelow)bya
doubleintegrationofthemeasuredaccelerationsignal:
BAtdtdttatx )()( Ascanbeseen,positionbasedonintegratedaccelerationcannotgiveinformationaboutmean
levelorpossibleconstantdriftoftheposition.Increasingperiodofoscillationwillgivereduced
accuracyofthederivedposition.Forpracticalapplicationsthismethodarethereforeusuallylimited
tomeasurementsofthewavefrequencypartofthemotions.
Anotherindirectwaytoestablishthepositionisusingmeasuredforceincombinationwithalinear
spring:
k
tF
tx
)(
)(
Themethodrequiresaspringconnectionbetweenthemodelandafixedpoint(e.gtowingcarriage,
seabedetc.).Itisnecessarythatthespringstiffnessissufficientlowtoavoidanyinfluenceonthe
dynamicbehaviorofthemodel.
4.4 Accelerations
Measurementsmadebyaccelerometersarebasedontheratiobetweenforce,massand
acceleration:
-
7/23/2019 Experimental Methods in Marine Dynamics
36/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page35
m
tFta
)()(
Amasscanbeconnectedtoabeam.Whenexposedtoaccelerationthebeamwillbedeflectedby
theinertiaforces.Thedeflectionofthebeamisproportionaltotheacceleration.Straingaugescan
beusedformeasuringthedeflectionofthebeamandhencetheaccelerationisobtained.
Anothertypeofaccelerometersisbasedonthepiezoelectricaleffect.Apiezoelectricalmaterialis
amaterialwhichwhendeformedproducesanelectricalfield.Thevoltagegeneratedisproportional
tothesurfacepressureapplied.Combinedwithamassthisgivesasignalproportionaltothe
acceleration.TheprincipleisshowninFigure4.9. Thechargeistransferredtovoltageinacharge
amplifier,butsomeofthechargeleaksout.Thisgivestheaccelerometeralowerlimitforwhich
frequenciesthatcanbecovered.Thistypeofaccelerometerscanthereforeonlybeusedfor
dynamicmeasurements.
Figure 4.9 Piezo electric material exposed to surface pressure.
Theresonanceofthemassspringsystemmayinfluencethemeasurementofaccelerations.Forfrequencieswellbelowtheresonancefrequencythemasswillfollowthemotionsofthehousing
andwehavealinerrelationbetweentheaccelerationandthesignalout.Forfrequenciesinthe
resonanceregionthemasswillbeexitedandthesignaloutwillbefrequencydependent.The
dynamicamplificationswillbedependentofthedampingofthesystem,butingeneral
accelerometersshouldonlybeusedformeasurementsofresponseswithoscillationfrequencies
wellbelowthenaturalfrequencyoftheaccelerometer. AccelerometersbasedonPiezoelectricity
canbemadeverystiffwithresonancefrequencyhigherthan500KHz.Thismakesthemusefulfor
applicationsofmeasurementsofresponseduetoimpactloads. Toincreasethesensitivityofthe
accelerometerthemassmustbeincreasedorthestiffnessreduced.Accelerometerswithlow
naturalfrequencywillthereforebemoresensitivethantheaccelerometerswithhighresonancefrequency.
Theaccelerometersaddweighttothestructureanditisthereforeimportanttoensurethatthat
weightissufficientlylowtoavoidanyinfluenceonthedynamicbehaviour.Theweightofthe
accelerometercanbemadeverysmall,typicallydowntoafewgrams.
4.5 PressureTransducers
Pressuremeasurementsaremostlyperformedusingpressurecells.Threetypesofpressurecellsarecommonlyused:
-
7/23/2019 Experimental Methods in Marine Dynamics
37/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page36
1. basedonpiezoelectricity
2. basedoninductivetransducers
3. basedonstraingauges.
Pressure
cells
are
basically
force
measurements
over
a
small
area.
Typical
dimensions
of
presser
cellsusedformodeltestingisD=210mm.Thedifferenttypesofpressuremeasuringdevicesare
illustratedinFigure4.10.
Figure4.10 Schematicrepresentationofthemostcommontypeofpressuretransducers.
(a):Capacitancetransducer, (b):Piezoelectricand(c):Straingauge
Pressurecellsbehaveinmanywayssimilarasanaccelerometerandtheresonanceofthemass
springsystemmayinfluencethemeasurements.Thedynamicamplificationswillbedependentof
thedampingofthesystem,butingeneralpressurecellsshouldonlybeusedformeasurementsof
responseswithfrequencieswellbelowthenaturalfrequencyofthecell. Straingaugetypecells
respondstodisplacementsfromdcto5kHz.Itisthereforewellsuitedformostpracticalmodel
testing.Pressurecellsbasedonpiezoelectricitycanbemadeverystiffwithresonancefrequency
uptomorethan500kHz. AnexampleofthistypeofpressurecellisshowninFigure4.11.This
transduceris
therefore
well
suited
to
measurements
of
pressure
behavior
with
very
low
rise
time
as
willbethecaseforslammingpressuremeasurements.Anexampleofmeasuredslammingpressure
fortheimpactofaflat,elasticplatetowardsawavecrestisshowninFigure4.12.Itisobserved
thatclosetothecenteroftheplatebottomwherethewavecresthit,therisetimeislessthan
0.0001sandthedurationofthepeakextremelyshort.Consequentlyapressurecellwithveryhigh
resonanceperiodwillberequiredtoaccuratelyreproducethispressurebehavior.
-
7/23/2019 Experimental Methods in Marine Dynamics
38/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page37
Figure 4.10 Piezoelectric pressure transducer for pressure measurements.
Figure 4.11
Example of measured slamming pressure. Impact of a horizontal circular cylinder
towards calm water surface.
4.5.1 Measurementofpressuredistribution
Inthe
later
years,
pressure
sensing
film
has
been
developed
by
several
different
companies.
The
filmisbasicallyamatrixofsmallpressurecellsintegratedintoaflexibleplasticfilmthatcanbe
appliedtocurvedsurfaces,andwilleffectivelyreturnthepressuredistributionoverthesurface.
Thepressurecellsaremadeofalayerofsemiconductingmaterialwherethedegreeof
conductivitydependsonthepressureappliedtothematerial.Twocompaniesthatdevelop
pressuresensingfilmareTekscanhttp://www.tekscan.com/andPressureProfileSystems
http://www.pressureprofile.com/.Thistechnologyhasmainlybeendevelopedfordry
applications,liketestinganddevelopmentofcarseats,sportsequipment,andsimilar.Thus,itisnot
straightforwardtoapplyittomarinehydrodynamicsproblems,butthepossibilityofeasily
measuringthepressuredistribution,notonlypointpressures,meansthatthistechnologyis
probablygoingtobeappliedalsotomarinehydrodynamicsinthefuture.
-
7/23/2019 Experimental Methods in Marine Dynamics
39/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page38
Aslightlysimilartechnologyispressuresensitivepaint(PSP).Thecolorofthepaintis
changingwiththepressure,whenaspeciallightsourceisused.Thisisalsoarecentmeasurement
technique,developedintheformerSovietUnionandknownintheWestsinceanadvertisementin
AviationWeeklyin1990.Itisprimarilyusedinwindtunneltestingofaircraft.Thepressure
sensitivepaintissensitivenotonlytopressure,buttotemperatureandoxygencontentintheflow,
somethingthatcomplicatestheapplication.
4.6 Velocities
Thevelocity inapointcanbeobtainedbyastraightforwardintegrationofmeasuredacceleration
orbyaderivationofmeasuredposition.Bothmethodsarecommonlyusedforvelocity
measurementsofstructuralcomponents.
Formeasurementoffluidvelocitydifferentprinciplesarepossible:
Basedonmeasurementsofpressure,e.g.pitottubes LDV
Ultrasonictransducers
Bymeasuringrateofrevolutionofasmallimpeller.
Thetwofirstmethodsarediscussedinthefollowing.
4.6.1 Pitottubes
Thepitottubesensoriscommonlyusedformeasurementofthewakesurveys,flowthroughwater
jetsetc.ThePrandtlpitottubeisshowninFigure4.13.Thepressuredifferencebetweenthetotal
pressureheadatthefront(inpos.Ainthefigure)andthestaticpressureattheside(atpositionB)
ismeasuredbyadifferentialpressurecell.Basicallythepitottubeisapressuredifferencemeasure,
butthevelocityisobtainedfromthewellknownrelation:
21 2p U
Toimproveaccuracythistheoreticalrelationisnotused,insteadthecalibratedrelationbetween
pressureandvelocitywillbeapplied.
-
7/23/2019 Experimental Methods in Marine Dynamics
40/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page39
Figure 4.12 Prandtl pitot tube.
Tocovermorepositionsinthesamerun,severalpitottubescanbemountedtogetherasshownin
Figure4.14.
Usingpitottubeswithfiveholeslocatedindifferentangularpositiononasphericalhead,the
velocityinallthreedirectionscanbemeasured,incaseofwakesurveys;axial,tangentialandradial
velocity.
Figure 4.13 Pitot tube arrangement for measurement of velocity in several positions.
-
7/23/2019 Experimental Methods in Marine Dynamics
41/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page40
4.6.2 LaserDopplerVelocimetry LDV
LaserDopplerVelocimetry(LDV)hasbeenusedformorethan20yearsformeasurementsofflow
aroundshipsandpropellers.Theusehasbeenmainlyforvalidationofpredictiontoolsforvelocity
distributionaroundliftingsurfaces,withinboundarylayersandforwakeflow.GenerallyLDV
measurementsaretimeconsumingandexpensivetoperformandtheuseforcommercialmodel
testinghave
been
very
limited.
See
ITTC,
(1996)
for
afurther
discussion
for
application
of
LDV
in
modeltesting.
LDVusestheDopplershiftinthereflectedlightfrequency(color)todeterminethevelocityand
directionoftheflow.Byusingtwobeamsfromdifferentdirection,the3Dvelocityvectorina
singlepointcanbemeasured.Tomeasurevelocityindifferentpositions,thetransmittingand
receivingopticsmustbemoved(seeFigure4.14).Thisiscommonlydoneusinganautomatic
traversingsystem.
OneofthemainbenefitsofLDVisthatitisanonintrusivemeasurementtechnique,whichmeans
thatone
does
not
have
to
put
any
sensors
into
the
area
where
one
wants
to
measure,
thus
one
is
notinterferingwiththeflowfieldofinterest.LDVdoalsogiveveryquickresponse,whichmeans
thatitissuitableformeasurementofturbulenceandsimilarlyrapidlychangingflowphenomena.
Formeasurementofaveragevelocityinonedirection,itisgenerallyrecommendedtousepitot
tubesorsimilartechniques.
ForLDVtoworkthereneedstobelightreflectingparticlesdissolvedinthewaterinorderto
providelightscattering.Ifthereisnoparticlesinthewaterthelightfromthelaserwillnotbe
reflected.Infact,oneisnotmeasuringthewatervelocity,butrathertheparticlevelocity.There
mightbesufficientdirtinthewaterfromthestart,butitiscommontohavetoapplyparticlesfor
thepurpose
of
LDV
measurement.
This
process
is
called
seeding.
Proper
seeding
is
one
of
the
keys
tosuccessfulapplicationofLDV.Whentestinginlargefacilities,likealargetowingtank,seeding
mightbeoneofthemainchallenges.Seedingtheentiretankisdifficultandexpensive.Seeding
locallyintheareaofmeasurementmightdisturbtheflow,anditmightbedifficulttoobtaina
reasonablyhomogeneousdistributionofparticles.
Figure 4.14 Principles of a LDV measurement system
Laser
Signal
processing
Transmitting
optics
Receiving opt ics
with detector
Signal
conditioner
Flow
HeNeAr-Ion
Nd:Yag
Diode
Beamsplitter(Freq. Shift)
Achrom. Lens
GasLiquid
Particle
Achrom. LensSpatial Filter
Photomultiplier
Photodiode
Spectrum analyser
Correlator
Counter, Tracker
Amplifier
Filter
PC
-
7/23/2019 Experimental Methods in Marine Dynamics
42/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page41
4.6.3 ParticleImageVelocimetry PIV
ParticleImageVelocimetry,orPIV,isanonintrusive,opticaltechniqueformeasurementofvelocity
vectors.AsforLDVlaserlightisused,andsimilartoLDVthewaterneedsparticlesseedingto
providelightscattering.WhileLDVmeasuresvelocityinasinglepointatatime,PIVmeasuresthe
velocityinanarea,soitisconsideredafieldmeasurementtechnique.PIVusesalaserlightsheet,
createdby
putting
aspreading
lens
in
front
of
the
laser
beam.
By
taking
two
stereo
photographs
(or
onedoubleexposurestereophotograph)withveryshorttimeintervalthevelocityoftheparticles
canbedeterminedfromhowfartheyhavemoved.Byusingstereophotographs,themovementin
space,notonlyinasingleplane,canbedetermined.PIVhasbeeninuseforalongtime,butitis
theadvanceindigitalhighspeedvideoandimageanalysisthatquiterecentlyhasmadePIV
interestingtoapplyinregularhydrodynamicsresearch.Inthetimeoneusedfilmbasedpictures
andmoreorlessmanualanalysis,PIVwasextremelytediousandtimeconsuming.Now,semi
automatinganalysisofthedigitalvideoimagesmeansthatlargeamountsofmeasurementdatacan
begeneratedfairlyquickly.Also,theaccuracyhasbeengreatlyincreased.PIVisincreasinglyused
insteadofLDV,sinceitismuchfastertomapavelocitydistributionactuallythedistributioninan
areaiscapturedatoneinstant,andnotoversometime,aswithLDV.
Figure 4.15 Principles of a PIV measurement system
4.7 Forcemeasurements Dynamometers
Theloadcellsusedinmodeltestingareoftendesignedtofitaspecificpurposeandtocoverthe
expectedrangeofloadsduringthetests.Forexamplefortowingtests,veryhighaccuracyin
measuredforcewillberequiredandthetransducerwillbetailormadetomeasureforceinone
directionwithahighaspossibleresolution.Thisiscalledaresistancedynamometerandisstandard
equipmentinatowingtank.InFigure4.15adynamometerformeasurementsofpropellerthrust
andtorquedirectlyonthepropellerhubisshown. Thethrustismeasuredbyaninductiveposition
transducerandthetorquebystraingaugeswhichmeasuresheardeformationonahollowpartof
thepropellershaft.
-
7/23/2019 Experimental Methods in Marine Dynamics
43/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page42
Figure 4.16 Dynamometer for measurements of propeller thrust and torque.
Transducersformeasurementsofforcesinoneormoredegreesoffreedomareoftenproducedas
apurposemachinedpiecewithstraingaugesgluedtothebasematerial.Atypicaldesignfor
measurementofforcesin3d.o.fs(axialforceandshearforces)isshowninFigure4.17.
Figure 4.17 Example of force transducer based on strain gauges. Axial forces and shear forces
are measured.
Themachiningofthematerialgivesareaswithhighshearstresseswherethestraingaugesare
mounted.Bycarefuldesignofthetransducerthecrosstalkcanbekeptataminimum.Cross
talkmeanscouplingeffectsbetweenthedifferentdegreesoffreedom.Forexampleforthe
transducerinFigure4.17,ifapuretensioninxdirectionisapplied,themeasuredresponsefrom
thetransducerinyandzdirectionisaresultofcrosstalk.Fortransducerdesignitisimportant
withminimumcrosstalk.
Using3transducerofthistypemountedbetweentwoplatesa6d.o.ftransducerisobtained.
4.8 WaveMeasurements
Waveelevationismostcommonlymeasuredbymeansofwaveprobesoftheconductive(or
resistance)type. Avoltageisappliedontoparallelrods.Theresistanceisdeterminedbythelength
-
7/23/2019 Experimental Methods in Marine Dynamics
44/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page43
oftherodswhichiswetted(orsubmerged).Bymeasuringthecurrentduetotheapplied
voltageacrosstherodsthewettedpartandhencesurfaceelevation,isdirectlyachieved. Arraysof
threeormoreofthistypeofsensorscanbeusedtomeasurethedirectionaldistributioninshort
crestedwaves.
Waveprobesarealsousedformeasurementofrelativemotionsbetweenthestructureandthe
watersurface.Thewavegaugemaythenbemountedonthestructureandtherelativemotionin
thepointisdirectlyobtained.ExamplesoftransducersolutionsforthispurposeareshowninFigure
4.18. Bothrodsandconductivetapegluedtothemodelareusedforthispurpose.Rodsare
preferableatzerospeedduetoeasiermountingandcalibration,whileconductivetapeisoften
requiredformodelswithforwardspeed,toavoidresistanceandwatersprayfromtherods.
Figure 4.18 Example of wave transducers for measurements of relative motions.
Formeasurementofwavesathighforwardspeeds,thewirebasedprobesdontworkwell,dueto
thesprayandwavemakingofthesurfacepiercingwires.Runupinfrontofthewiresand
ventilationbehindthewiresleadstolargeerrorsinthemeasurements.Forforwardspeedsofmore
than2m/s,thewirebasedprobesshouldnotbeused.Alternativesaremainly:
Ultrasoundwaveprobes
Servoneedlewaveprobes
Ultrasoundwaveprobesworksbysendingoutahighfrequencysoundpulse,andmeasuringthe
timeittakesbeforethereflectedsoundwavereachestheprobe.Thetechniquehasbeenusedfor
alongtimeforlevelmeasurementintanksanddams,butitisnotuntilfairlyrecentlythat
instrumentswithsufficientaccuracyfortowingtankwavemeasurementhasbeenavailable.The
UltraLabsystems
from
General
Acoustics
is
in
practical
use
in
the
hydrodynamic
laboratories
at
the
MarineTechnologyCentre.Someofthesesystemshavelimitationswithrespecttoforwardspeed
-
7/23/2019 Experimental Methods in Marine Dynamics
45/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page44
andwavesteepness,whilethemostadvancedsystemscoverallconditionsofpractical
interestfortowingtankwork.
Servoneedlewaveprobesconsistofasensingneedlemountedonaservomechanism.Thesensing
needlemeasuresthedegreeofcontactwiththewater,andtheservomechanismmakessurethe
needlehasafairlyconstantsubmergence.Then,theactualwaveheightisfoundbymeasuringthe
positionoftheneedle.Thisisafairlycomplexandfragileinstrument,andtheonlyreasontouse
suchaninstrumentisthecapabilityofwavemeasurementathighforwardspeed.
4.9 DataAcquisition
Thedifferentinstrumentsappliedinthetestsetupareconnectedbycablestoadataacquisition
systemtorecordthemeasureddata.AschematicofadataacquisitionsystemisshowninFig4.1.
4.9.1 Amplifiers
Atypicalanalogtransducersignaliswithoutputinmicrovolts.Itisthereforeamplifiedbyan
amplifier,usuallyto+/10Voltrange.
Dependingontypeoftransducerdifferenttypeofamplifiersisused.Amplifiersforanalogsignals
fromstraingaugeandsimilartypeoftransducerscanhavebridgeexcitationandbridgebalancing
builtin.Thismeansthattheamplifierwillprovidethecurrentandvoltagerequiredforthe
measurementbridge(seesection4.2.1Straingauges),inadditiontoamplificationoftheoutput
signal. Piezoelectricaltransducersrequireachargeamplifier. Inductiontypetransducersrequire
ACexcitation,whichmeansthatthedrivingcurrentofthetransducerisACratherthanDC.Strain
gaugetransducerscanuseeitherACorDCexcitation.
4.9.2
Filters
Filterscanbeeitheranalogordigitalfilters.Analogfiltersareappliedbeforethesignalsare
convertedtodigitalunitsbytheADconverterandmaybebuiltinasanintegratedpartofthe
amplifier.ThedigitalfiltersareappliedaftertheADconversionandcanbeimplementedeitherasa
digitalcircuitorassoftwareinthecomputerusedforanalysis.
Thefiltersremovesignalsatcertainfrequencybands.Dependingonwhichfrequencybandis
removedtheycanbesplitintothreeclasses:
Lowpass,i.e.forremovingofhighfrequencycomponents
Highpass, i.e.forremovingoflowfrequencycomponents
Bandpass
thedifferenttypesareillustratedinFigure4.19.
Analoglowpassfilteriscommonlyusedforremovingofnoiseasthenoiseisusuallyappearingata
significantlyhigherfrequencythanthephysicalmeasuringsignal. ToavoidNyquistphenomena(se
discussionbelow)thecutofffrequencyoftheanaloglowpassfilteredshouldbesettobelower
thanhalfthesamplingfrequencyfS..Thegeneralrecommendationistosetthecutofffrequency
muchlowerthanhalfthesamplingfrequency1/10ofthesamplingfrequencyisthepreferredvalue,butitmightmeanthathighsamplingfrequenciesarerequired,andthereforecompromises
areoftenmade.
-
7/23/2019 Experimental Methods in Marine Dynamics
46/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page45
Figure 4.19 Illustration of different type of filters.
Lowpassfiltersappliedinrealtimecausesatimedelay.Thismightbeillustratedwithanexampleofaverysimplelowpassfilter,whichiscreatedbycreatingthelowpassfilteredsignalfroman
averageoftheunfilteredsignaloveracertainperiodoftime.Intheexample,showninFigure4.20,
asinusoidalsignalwithperiodof30secondshashadanothersinusoidalsignalwithperiod1.2
secondssuperimposed.Thefilterisimplementedasarunningaverageover2.4seconds,seenin
Figure4.20asthetimeittakesbeforethefilteredsignalappears.Itisclearlyseenfromthefigure
thatthefilteredsignallagsbehind,withhalftheaveragingtime.Thelongertheaverageperiod,the
lowerthefilterfrequency,andthelongerthetimedelay.Iftheaveragingwindowcouldhavebeen
symmetricallyplacedrelativetothetimeofthefilteredvaluethedelaywouldbeavoided.Thiscan
beachievedwhenfilteringanexistingdataset,butnotwhenfilteringinrealtime,sinceitwould
requiretheabilitytolookintothefuture.
Itshouldbenotedthatfilteringisinpracticenotperformedbysimpleaveraging.Thereisalarge
varietyofmethods,whichisnotcoveredhere.SeeforinstanceDunn(2005)foradiscussionof
filteralgorithms.
Amplitude
Frequency
Ideal characteristic
Real characteristic
Low pass filter
High pass filter
Band pass filter
-
7/23/2019 Experimental Methods in Marine Dynamics
47/182
LecturenotesinExperimentalMethodsinMarineHydrodynamics,issuedAugust2014
Page46
Figure 4.20Illustration of time-delay due to filtering
4.9.3 AnalogtoDigital(AD)Conversion
Mosttransducertypes,includingthelargegroupofstraingaugebasedtransducers,areanalog
transducers,meaningthattheyproduceananalogoutputsignal.Torepresentthissignalina
computerit
has
to
be
digitized.
The
process
of
digitalization
is
performed
in
the
AD
converter.
TheADconverterisusuallyaphysicallyseparateunit;aboxoranextracardforthecomputer.The
lineinpartofacomputersoundcardisanADconvertercustommadeforsound,butreallyquite
similartotheADconvertersusedforothermeasurements.TheADconverterunitwilloftenalso
haveapossibilityfordigitaltoanalogconversionDAsimilartothelineoutofacomputersound
card.TheDAconvertermightforinstancebeusedtoproduceasignalforacontrolsystem.TheAD
convertermightbeintegratedwiththemeasurementamplifier.ThisisthecasefortheHottinger
MGC+digitalmeasurementamplifiersinuseinthehydrodynamiclaboratoriesattheMarine
TechnologyCentre.
TheADconverterunitwill,dependingontheactualmodel,haveacertainnumberofchannels,
whichmeanshowmanysignalscanbeconvertedsimultaneously.LimitationsintheADconverter
willdeterminehowfastthedatacanbesampledthesamplingfrequency.Itmeansthatfor
experimentsrequiringveryfastsampling,specialADconverterequipmentmighthavetobe
acquired.
OneshouldalsobeawarethatsomeADconverterssampleallchannelsatexactlythesameinstant,
whileotherswillsamplethechannelssequentiallyduringthesamplinginterval.Ifforinstance10
channelsaresampledat10Hz,thesequentialADconverterwillsampleasinglechannelevery
1/100second,
so
that
each
channel
is
sampled
every
1/10
second,
but
not
at
the
same
time.
This
is
usuallynotaproblem,sincet