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Thermodynamics of surfaces and interfaces
Atkins (ed. 10 and 11): §16C C.4 Atkins (ed. 9): § Atkins (ed. 8): § Study Guide: P.14
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Na2ClO3 crystals in solution
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Large crystals grow; small crystals dissolve
T = 1 day 3
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Large crystals grow; small crystals dissolve
Wilhelm Ostwald Ostwald ripening (1896) T = 0 T = 1 day 4
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Equilibrium: one single crystal
T = 1 day 10 days 30 days 5
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Equilibrium: one single crystal
T = 1 day 10 days 30 days 6
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Gibbs-Thomson effect Interfacial (free) energy between two phases
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Gibbs-Thomson effect Interfacial (free) energy between two phases
relevant for P >1 P =1 P =2,3 P =2,3
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Laplace equation: γ surface free energy (Jm-2)
out in Equilibrium:
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Laplace equation γ r γ r+dr equilibrium Laplace equation
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Surface tension γ (Jm-2 = Nm-1)
water
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Surface tension and capillary action
Pressure of liquid column of height h Laplace equation equilibrium capillary action Adhesive force between fluid and capillary
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Surface tension and capillary action
γ counteracts the adhesion between liquid or gas and capillary
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Surface tension and wetting
specific work (J/m2) of adhesion (γ is always trying to reduce the corresponding surface) horizontal Force (N/m) balance (equilibrium)
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Surface tension and wetting
} Work (J/m2) Force (N/m) partial dewetting partial wetting
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Kelvin equation (nucleation barrier for condensation (g l))
γ Pout Laplace equation Pin l g equilibrium constant T Kelvin equation small droplets evaporate condensation nucleation barrier Pg > P*
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nucleation of phase α(l) from phase β(s)
revert to Gibbs free energy classical nucleation theory spherical nucleus, radius r driving force: surface free energy: γ molar volume: Vm γ β α Free energy gain cost
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nucleation barrier depends on supersaturation
nucleation barrier and critical radius Δμ Δμ Δμ Δμ Δμ nucleation barrier depends on supersaturation (Δμ = Δμ(T)) -low Δμ : no nucleation -high Δμ : easy nucleation
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