Thermomolecular Pressure in Surface Melting: Motivation for Frost Heave
J. G. DASH 1
1 Department of Physics, FM-15, University of Washington, Seattle, WA 98195.
A thermomolecular pressure is associated with surface melting, and it can drive mass flow along an interface under a lateral temperature gradient. The pressure is a universal thermodynamic function in the limit of thick films. It may be responsible for frost heave in frozen ground.
Submitted on August 4, 1989
Accepted on October 13, 1989