Capillary Surface Tension

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    Colloidal Dispersions 2005

    Surface and Interfacial Tensions

    Lecture 1

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    Surfaces and Interfaces 1Colloidal Dispersions 2005

    Surface tension is a pull

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    Surfaces and Interfaces 2Colloidal Dispersions 2005

    Thermodynamics for Interfacial Systems

    F A =

    Work must be done to increase surface area just as work must be done

    to compress a gas.

    At constant temperature (T), volume (V) and composition (n), the

    energy, F, necessary to increase the surface area by an amount, A,is:

    Where is the surface tension.

    When Fis negative, the process is spontaneous.When Fis positive, the process reverses.

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    Surfaces and Interfaces 3Colloidal Dispersions 2005

    Coalescence of Droplets

    The change in energy is:

    +

    ( )

    0

    final initial

    final initial

    F F F

    A A

    A

    =

    =

    =

    +

    This is not the common assertion.

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    Surfaces and Interfaces 6Colloidal Dispersions 2005

    Works of Cohesion and Adhesion

    12 1

    2

    11

    1 2 12

    adhW = +

    12

    coh

    W =

    The work of adhesion is the

    separation to create two new

    surfaces from one interface:

    The work of cohesion is theseparation to create two new

    surfaces.

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    Surfaces and Interfaces 7Colloidal Dispersions 2005

    Liquids have different contact angles on different solids

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    Surfaces and Interfaces 8Colloidal Dispersions 2005

    Contact angles: Liquids on solids

    The contact angle of 140o is the same for each drop, independent of

    drop size.

    The observation is that the contact angle depends on the materials but

    not the particular geometry.

    Mercury drops on glass.*

    Drops vary in size from 4 to 24grains (1 grain = 64.8 mg)

    * Bashforth and Adams, 1883.

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    Surfaces and Interfaces 9Colloidal Dispersions 2005

    The interaction of a liquid and a solid

    = +cossv lv sl

    The Young-Dupr introduces the idea of a solid surface/vapor surface

    tension, sv and a solid/liquid interfacial tension, sl.

    sv

    lv

    sl

    The idea is that the three

    tensions are balanced:

    A sessile liquid drop on a

    solid:

    The contact angle is and is assumed to be independent of the geometry.

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    Surfaces and Interfaces 10Colloidal Dispersions 2005

    The Molecular Origin of Surface Tension

    The molecules at the

    liquid surface are pulled

    towards the bulk liquid.

    To expand the surface

    requires work. The workis the surface tension

    times the change in

    area.

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    Surfaces and Interfaces 11Colloidal Dispersions 2005

    The Molecular Origin of Interfacial Tension

    = + 1 2 12adhW

    The stronger the interfacial

    interactions, the lower the

    interfacial tension!

    But the greater the work of

    adhesion:

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    Surfaces and Interfaces 12Colloidal Dispersions 2005

    A theory for interfacial tensions

    Liquid 1

    Liquid 2

    1

    2

    1 2

    d d

    1 2

    d d

    12 1 2 1 22d d = +

    Fowkes, in Ross, ed. 1965, p. x

    The adhesion between the

    liquids is approximated by the

    root-mean-square of the

    surface tensions:

    1 22adh d d

    W =

    hence

    The superscript d refers to the dispersion or van der Waals types of attraction.

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    Surfaces and Interfaces 13Colloidal Dispersions 2005

    Large surface heterogeneities - contact angle

    hysteresis

    Advancing liquids are held up by low energy spots and

    show high contact angles.

    Receding liquids are held by high energy spots and

    show low contact angles.

    High energy spots

    low contact angles.

    Low energy spots

    high contact angles.

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    Surfaces and Interfaces 14Colloidal Dispersions 2005

    Small heterogeneities - contact angle changes

    Coverage

    0.0 0.2 0.4 0.6 0.8 1.0

    cos

    w

    0.0

    0.2

    0.4

    0.6

    0.8

    1.0

    The cosine of the static contact angle of water on varioussubsaturated monolayers plotted versus the surface coverage

    measured directly using the atomic force microscope.

    Text, p. 220.

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    Surfaces and Interfaces 15Colloidal Dispersions 2005

    Motion of liquids due to surface energies

    Capillary flow

    Motion as a consequence of shape.

    Key idea: pressure drop across a curved

    surface

    Marangoni flow

    Motion as a consequence of variation insurface tension.

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    Surfaces and Interfaces 16Colloidal Dispersions 2005

    Pressure drops across a curved surface

    R1

    R2

    x x+dx

    dz

    y

    y+dy

    1 2

    1 1Lp

    R R

    = +

    The pressure is larger on the concave (inside) of the curved surface.

    The Laplace equation:

    R1 and R2 are the radii of curvature.

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    Surfaces and Interfaces 17Colloidal Dispersions 2005

    Bubbles are difficult to nucleate

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    Surfaces and Interfaces 18Colloidal Dispersions 2005

    Ostwald Ripening

    The pressure inside > pressure outside

    2p

    r

    =

    This equation implies that in an emulsion with a range of drop sizes or

    a foam with a range of bubble sizes, material diffuses from small

    drops to large drops.

    Also, this equation implies that bubbles are difficult to nucleate.

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    Surfaces and Interfaces 19Colloidal Dispersions 2005

    The Kelvin Equation

    2ln m

    o

    P V

    P rRT

    =

    0

    2ln m

    c V

    c rRT

    =

    Similarly for small particles in suspension. If the particles have any

    solubility, the small particles become smaller and the large particles

    become larger. The effect is described by the Kelvin equation.

    All these processes are called Ostwald ripening.

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    Surfaces and Interfaces 20Colloidal Dispersions 2005

    Capillary rise is another example of Laplace pressure

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    Surfaces and Interfaces 21Colloidal Dispersions 2005

    Capillary rise

    The final position is determined by 2 principles:

    (1) The pressure drops across curved interfaces.

    (2) The pressure in the liquid must be the sameat the same depth.

    In the final state the pressure drop across the ACinterface equals the hydrostatic pressure from C to B.

    2 co sLg hR

    =

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    Surfaces and Interfaces 22Colloidal Dispersions 2005

    Marangoni Flow

    Marangoni flow

    flow resulting from local differences in

    surface tension.

    Causes of Variation in Surface Tension

    Local temperature differences.

    Local differences in composition due to

    differential evaporation.

    Electric charges at surfaces.

    Local compression or dilatation of

    adsorbed films.

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    Surfaces and Interfaces 23Colloidal Dispersions 2005

    Liquid will flow away from a low surface tension region

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    Surfaces and Interfaces 24Colloidal Dispersions 2005

    Liquid flows to the higher surface tension

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    Surfaces and Interfaces 25Colloidal Dispersions 2005

    Tears of Wine

    +

    EthOH/H O2

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    Surfaces and Interfaces 26Colloidal Dispersions 2005

    Flow due to surface tension differences

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    Surfaces and Interfaces 27Colloidal Dispersions 2005

    Liquid flows away from a hot spot

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    Surfaces and Interfaces 28Colloidal Dispersions 2005

    Liquid flows to a cold spot

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    Surfaces and Interfaces 29Colloidal Dispersions 2005

    Equations of Capillarity

    , , iT V n

    F

    A

    =

    = +cosSV LV SL

    1 2

    1 1pR R

    = +

    ( )grad = +

    Surface Free Energy

    Young-Dupr Equation

    LaPlace Equation

    Marangoni Flow