My watch list
my.chemeurope.com  
Login  

Kelvin equation



Kelvin equation describes the change of vapour pressure over liquid curved with a radius r (for example, in a capillary or over a droplet). The Kelvin equation is used for determination of pore size distribution of a porous medium using adsorption porosimetry.

\ln {p\over p_0}= {2 \gamma V_m \over rRT}
Where:
p - actual vapour pressure 
p0 - saturated vapour pressure
γ - surface tension
Vm - molar volume
R - universal gas constant
r - radius of the droplet
T - temperature

Additional recommended knowledge

Equilibrium vapor pressure depends on droplet size. If p0 < p, then liquid evaporates from the droplets.

If p0 >p , then the gas condenses onto the droplets… and they grow.

As r increases, p decreases and the droplets grow into bulk liquid.

If we now cool the vapour, then T decreases, but so does p0 . This means p/p0 increases as the liquid is cooled. We can treat γ and V as approximately fixed, which means that the critical radius r must also decrease. The further you supercool a vapour, the smaller the critical radius becomes. Ultimately it gets as small as a few molecules and the liquid undergoes homogeneous nucleation and growth.

See also

References

  • W. T. Thomson, Phil. Mag. 42, 448 (1871)
  • S. J. Gregg and K. S. W. Sing, Adsorption, Surface Area and Porosity, 2nd edition,Academic Press, New York, (1982) p.121
  • Adamson and Gast, Physical Chemistry of Surfaces, 6th edition, (1997) p.54


 
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Kelvin_equation". A list of authors is available in Wikipedia.
Your browser is not current. Microsoft Internet Explorer 6.0 does not support some functions on Chemie.DE