The Kelvin equation describes the change in vapour pressure due to a curved liquid/vapor interface (meniscus) with radius (for example, in a capillary or over a droplet). The vapor pressure of a curved surface is higher than that of a flat and non-curved surface. The Kelvin equation is dependent upon thermodynamic principles and does not allude to special properties of materials. It is also used for determination of pore size distribution of a porous medium using adsorption porosimetry. The equation is named in honor of William Thomson, also known as Lord Kelvin.
The Kelvin equation may be written in the form
where is the actual vapour pressure, is the saturated vapour pressure, is the surface tension, is the molar volume of the liquid, is the universal gas constant, is the radius of the droplet, and is temperature.
Equilibrium vapor pressure depends on droplet size.
- If , then liquid evaporates from the droplets
- If , then the gas condenses on to the droplets increasing their volumes
As increases, decreases and the droplets grow into bulk liquid.
If we now cool the vapour, then decreases, but so does . This means increases as the liquid is cooled. We can treat and as approximately fixed, which means that the critical radius must also decrease. The further a vapour is supercooled, the smaller the critical radius becomes. Ultimately it gets as small as a few molecules and the liquid undergoes homogeneous nucleation and growth.
The change in vapor pressure can be attributed to changes in the Laplace pressure. When the Laplace pressure rises in a droplet, the droplet tends to evaporate more easily.
When applying the Kelvin equation, two cases must be distinguished: A drop of liquid in its own vapor will result in a positively curved liquid surface or a bubble of vapor in a liquid, will result in a negatively curved liquid surface.
The form of the Kelvin equation in this article is not the form in which it appeared in Lord Kelvin's article of 1871. The derivation of the form that appears in this article from Kelvin's original equation was presented by Robert von Helmholtz (son of German physicist Hermann von Helmholtz) in his dissertation of 1885. That derivation is reproduced (in English) on the "Talk" page of Wikipedia's article on the Ostwald-Freundlich equation.
- Robert von Helmholtz (1886) "Untersuchungen über Dämpfe und Nebel, besonders über solche von Lösungen" (Investigations of vapors and mists, especially of such things from solutions), Annalen der Physik, 263 (4) : 508-543. On pages 523-525, Robert von Helmholtz converts Kelvin's equation to the form that appears here (which is actually the Ostwald-Freundlich equation).
- Sir William Thomson (1871) "On the equilibrium of vapour at a curved surface of liquid," Philosophical Magazine, series 4, 42 (282) : 448-452.
- S. J. Gregg and K. S. W. Sing, Adsorption, Surface Area and Porosity, 2nd edition, Academic Press, New York, (1982) p.121
- Arthur W. Adamson and Alice P. Gast, Physical Chemistry of Surfaces, 6th edition, Wiley-Blackwell (1997) p.54
- Butt, Hans-Jürgen, Kh Graf, and MichaelThe Kappl. "The Kelvin Equation." Physics and Chemistry of Interfaces. Weinheim: Wiley-VCH, 2006. 16-19. Print.