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    ZETA POTENTIALZETA POTENTIAL

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    OutlineOutline

    1) Charge Development at Solid Interfaces2) Electrical Double Layers

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    Origin of Surface ChargeOrigin of Surface Charge

    Immersion of some materials in an electrolyte solution. Twomechanisms can operate.

    (1) Dissociation of surface sites.

    OH H

    OH

    OH OH

    OO

    O OO O

    OO O

    2

    OH

    sorpt on o ons rom so ut on.

    M

    OO O

    + + +

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    Origin of Surface ChargeOrigin of Surface Charge

    lattice cations or anions on surface, eg. AgI, BaSO4,

    (4) Surface charge due to crystal lattice defects, eg. lattice

    HO O O O OH

    Si

    HO O

    Al

    O

    Si

    O

    Si

    OH

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    Other Surfaces with ChargeOther Surfaces with Charge

    made of a self organizing

    lipid bi-layer. Most of the

    -

    negative charged.

    Oil dro lets develo

    Bubbles develop negative

    negative charge.

    charge since cationic species

    are more mobile, than anionic

    species and accumulate to the

    n er ace.

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    Electrical Double LayerElectrical Double Layer

    - Water moleculesx

    Distance from Surface

    +

    -

    -

    -

    +

    +

    -

    -Surface

    Counter-Ions

    --

    0

    otent a

    Co-Ions

    Helmholtz 100+ ears a o ro osed that surface char e

    is balanced by a layer of oppositely charged ions

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    GouyGouy--Chapman Model 1910Chapman Model 1910--19131913

    x--

    Distance from Surface

    +

    -

    -

    + +

    --

    -

    --0

    Assumed Poisson-Boltzmann distribution of ions from surface

    ions are point charges

    ions do not interact with each other

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    Stern (1924) / Grahame (1947) ModelStern (1924) / Grahame (1947) Model

    Diffusion layer-

    -

    x

    ++

    -

    -

    + +

    -

    -

    -

    +

    --

    -

    Shear Plane Gouy Plane Bulk SolutionStern Plane

    -

    -

    0

    Gouy/Chapman diffuse double layer and layer of adsorbed

    -

    charge

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    Salt AdditionSalt Addition

    Diffusion layer-

    -

    x

    Original Curve

    ++

    -

    -

    ++

    -

    -

    -

    +

    --

    -

    +

    Shear Plane Bulk SolutionStern Plane

    -

    -

    0+

    Gouy Plane

    -

    Salt will not effect the value of

    but will effect the value of

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    Salt AdditionSalt Addition

    +Diffusion layer-

    -

    x=0

    Original Curve

    +

    +

    +

    -

    -

    -

    +

    ++

    --

    -

    +

    + + --

    +

    Shear Plane Bulk Solution

    -

    -0

    Gouy Plane

    Stern Plane

    .

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    Debye Length: EDL ThicknessDebye Length: EDL Thickness

    Debye-Hckel parameter () describes the decay length

    1

    2

    0

    n

    i

    ii

    r

    ZC

    kT

    e

    Zi = electrolyte valence

    e = elementary charge (C)

    Ci = ion concentration (#/m3)n = number of ions

    =r

    0 = permittivity of a vacuum (F/m)

    k = Boltzmann constant (J/K) = temperature

    -1

    Deb e len th has units o len th

    Z P i l Eff f H

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    Zeta Potential Effect of pH

    OH-H+

    ++Shear+

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -+

    -

    +

    -+

    -

    +

    -+

    -

    +

    ShearPlane

    ShearPlane

    -

    +

    -

    +

    Low pH: Not-

    High pH: Not+

    There is a point that-

    there is a excess

    positive charge.

    is a excess negative

    charge.

    and H+ to completely

    balance out the

    sur ace c arge

    Z t P t ti l Eff t f H

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    Zeta Potential Effect of pH

    +

    -

    +

    -

    +

    -

    +

    + Isoelectric Point (IEP):-

    +

    -

    +

    -

    +V)

    +

    -

    +

    -

    pH(

    +

    -

    +

    -

    +

    -

    +

    -

    +

    -

    +-

    +

    -+

    -

    +

    -

    +

    -

    +-

    Z P i l Eff f H

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    Zeta Potential Effect of pH

    Question: What will happen to a mixed suspension of Alumina and

    3 4 ,

    ii

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    Zeta PotentialZeta Potential

    Increasing50

    ---- ----

    . .ZetaP

    20

    30

    tential( 0

    10

    V)

    -20-10

    -50

    -40

    -

    Alumina

    pH1 2 3 4 5 6 7 8 9 10 11

    Specific AdsorptionSpecific Adsorption

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    Specific AdsorptionSpecific Adsorption

    by electrostatics Have the abilit to shift the isoelectric oint

    Can reverse zeta potential

    Types of Specific Adsorption Ions Multivalent ions: Ca+2, Mg+2, La+3, hexametaphosphate,

    sodium silicate

    -

    Polyelectrolytes

    +

    ++

    +2+

    +

    +

    + +

    +

    +

    - - - - -

    S ifi Ad tiS ifi Ad ti

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    Specific AdsorptionSpecific Adsorption

    PO 3-

    Ca2+

    pH

    Multivalent anions shift IEP to left (apatite supernatant)

    Amankonah and Somasundaran, Colloids and Surfaces, 15, 335 (1985).

    El t ki ti PhEl t ki ti Ph

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    Electrokinetic PhenomenaElectrokinetic Phenomena

    E ectrop ores s

    Movement of particle in a stationary fluid by an applied

    e ec r c e .

    Movement of liquid past a surface by an applied electric field

    Streaming Potential

    charged surface

    Sedimentation Potential

    Creation of an electric field when a charged particle moves

    relative to stationary fluid

    Zeta Potential MeasurementsZeta Potential Measurements

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    Zeta Potential MeasurementsZeta Potential Measurements

    Electrophoresisdetermined b the rate of diffusion electro hroretic

    mobility) of a charged particle in a applied DC electric field.

    PCS determined by diffusion of particles as measured by photoncorrelation spectroscopy (PCS) in applied field

    Acoustophoresis determined by the potential created by a

    particle vibrating in its double layer due to an acoustic wave

    Streaming Potential determined by measuring the potential created as a fluidmoves past macroscopic surfaces or a porous plug

    Zeta Potential Meas rementsZeta Potential Meas rements

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    Zeta Potential MeasurementsZeta Potential Measurements

    assumed a >> 1 = Debye length

    a = particle radiuse ectr ca ou e ayer t c ness muc sma er t an part c e

    v = velocity

    r= media dielectric constant0 = permittivity of free space

    =

    0rv

    = medium viscosity

    E = electric field

    0r E = e ectrop oret c mo ty

    Zeta Potential MeasurementsZeta Potential Measurements

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    Zeta Potential MeasurementsZeta Potential Measurements

    Henry Formula (1931)ex anded for arbitrar a

    assumed E field does not alter surface charge density (o)

    - low 0

    r = media dielectric constant

    0 = permittivity of free space)a(f2

    v 10r

    = zeta potential = medium viscosity

    E = electric field)a(f

    3

    21

    0r

    E = electrophoretic mobility

    Hunter, Foundations of Colloid Science, p. 560

    Zeta Potential MeasurementsZeta Potential Measurements

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    Zeta Potential MeasurementsZeta Potential Measurements

    = Debye parametera = particle radius

    = zeta potential1

    a

    pE 0r

    = Potential over ca illar VE

    r= media dielectric constant

    0 = permittivity of free space (F/m) = medium viscosity (Pas)KE= solution conductivity (S/m)

    p = pressure rop across cap ary a

    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

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    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

    Electrophoresis - Zeta Mark 21particles ~ .10 microns- 300 m

    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

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    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

    Electroacoustic - Colloidal Dynamics Acoustosizer

    owders/slurries < 10nm - u to 50 wei ht%

    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

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    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

    -

    msuspensions

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    Equipment for Measuring Zeta PotentialEquipment for Measuring Zeta Potential

    tream ng otent a aar ys ca granu ar

    particles, surfaces