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Colloidal Dispersions © 2005 Surface and Interfacial Tensions Lecture 1

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Page 1: Lecture 1 Surfaces and Interfaces - Colloidal Dispersions in... · Colloidal Dispersions © 2005 Surfaces and Interfaces 1 Surface tension is a pull. Colloidal Dispersions © 2005

Colloidal Dispersions © 2005

Surface and Interfacial Tensions

Lecture 1

Page 2: Lecture 1 Surfaces and Interfaces - Colloidal Dispersions in... · Colloidal Dispersions © 2005 Surfaces and Interfaces 1 Surface tension is a pull. Colloidal Dispersions © 2005

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 Aσ∆ = ∆

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 σ is the surface tension.

When ∆F is negative, the process is spontaneous.When ∆F is 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 FA AA

σσ

∆ = −

= −

= ∆<

Therefore the drops coalesce spontaneously.

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Surfaces and Interfaces 4Colloidal Dispersions © 2005

Coalescence of Droplets with Emulsifier

+

When droplets covered with emulsifier coalesce, some emulsifier must be desorbed. This requires work.

work of desorptionF Aσ∆ = ∆ +

If the emulsifier is strongly adsorbed, the work to remove it is large, and the drops do not coalesce.

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Surfaces and Interfaces 5Colloidal Dispersions © 2005

Spreading of One Liquid on Another

The energy change per unit area for liquid 2 (top) to spread across the surface of liquid 1 (bottom) is: 2 12 1 ( )

final initialF F Fσ σ σ

∆ = −

= + −

The top liquid will spread when: 1 2 12σ σ σ> +

This is not the common assertion.

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Surfaces and Interfaces 6Colloidal Dispersions © 2005

Works of Cohesion and Adhesion

σ12σ1σ2

σ1σ1

1 2 12adhW σ σ σ= + −

12cohW σ=

The work of adhesion is the separation to create two new surfaces from one interface:

The work of cohesion is the separation 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 24 grains (1 grain = 64.8 mg)

* Bashforth and Adams, 1883.

Page 10: Lecture 1 Surfaces and Interfaces - Colloidal Dispersions in... · Colloidal Dispersions © 2005 Surfaces and Interfaces 1 Surface tension is a pull. Colloidal Dispersions © 2005

Surfaces and Interfaces 9Colloidal Dispersions © 2005

The interaction of a liquid and a solid

σ σ θ σ= +cossv lv sl

The Young-Dupré introduces the idea of a solid surface/vapor surface tension, σsv and a solid/liquid interfacial tension, σsl.

σsv

σlv

σslθ

The idea is that the three tensions are balanced:

A sessile liquid drop on a solid:

The contact angle is θ 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 work is the surface tension times the change in area.

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Surfaces and Interfaces 11Colloidal Dispersions © 2005

The Molecular Origin of Interfacial Tension

σ σ σ= + −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 2d dσ σ

1 2d dσ σ

12 1 2 1 22 d dσ σ σ σ σ= + −

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 dW σ σ=

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

Coverage0.0 0.2 0.4 0.6 0.8 1.0

cos θw

0.0

0.2

0.4

0.6

0.8

1.0

The cosine of the static contact angle of water on various subsaturated 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 curvedsurface

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 Rσ

∆ = +

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 outside2prσ

∆ =

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 VP rRT

σ =

0

2ln mc Vc rRT

σ =

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 same at the same depth.

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

2 c o sL g hR

σ θ ρ=

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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 todifferential evaporation.

Electric charges at surfaces.

Local compression or dilatation ofadsorbed 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”

σ+

σ

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

FA

∂ σ∂

=

σ σ θ σ= +cosSV LV SL

1 2

1 1pR R

σ

∆ = +

( )grad α βσ τ τ= +

Surface Free Energy

Young-Dupré Equation

LaPlace Equation

Marangoni Flow