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Ostwald–Freundlich equation

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Through Phase (matter), Surface tension and Vapor pressure

The Ostwald–Freundlich equation for a droplet or particle with radius R is:

ppeq=exp⁡(RcriticalR)
Rcritical=2⋅γ⋅VatomkB⋅T
Vatom = atomic volume
kB = Boltzmann constant
γ = surface tension (J ⋅ m−2)
peq = equilibrium partial pressure (or chemical potential or concentration)
p = partial pressure (or chemical potential or concentration)
T = absolute temperature

One consequence of this relation is that small liquid droplets (i.e., particles with a high surface curvature) exhibit a higher effective vapor pressure, since the surface is larger in comparison to the volume.

Another notable example of this relation is Ostwald ripening, in which surface tension causes small precipitates to dissolve and larger ones to grow. Ostwald ripening is thought to occur in the formation of orthoclase megacrysts in granites as a consequence of subsolidus growth. See rock microstructure for more.

History

In 1871, Lord Kelvin (William Thomson) obtained the following relation governing a liquid-vapor interface:

p(r1,r2)=P−γρvapor(ρliquid−ρvapor)(1r1+1r2),

where:

p(r) = vapor pressure at a curved interface of radius r
P = vapor pressure at flat interface (r=∞) = peq
γ = surface tension
ρvapor = density of vapor
ρliquid = density of liquid
r1 , r2 = radii of curvature along the principal sections of the curved interface.

In his dissertation of 1885, Robert von Helmholtz (son of the German physicist Hermann von Helmholtz) derived the Ostwald–Freundlich equation and showed that Kelvin's equation could be transformed into the Ostwald–Freundlich equation. The German physical chemist Wilhelm Ostwald derived the equation apparently independently in 1900; however, his derivation contained a minor error which the German chemist Herbert Freundlich corrected in 1909.

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