Based on the equilibrium, continuity and energy principles of the multi-pha
se porous medium, the heat-moisture-deformation (HMD) coupling model is est
ablished for the frozen soil foundation in this paper, with the considerati
on of the force interaction between the soil skeleton and ice particle, and
the energy jump behaviors during the phase-changing between ice and water.
A numerical solution with FEM using the proposed model is developed on the
plate of the Austrian software FINAL (Li and Chen, 1999) and a test calcul
ation with the new developed model is also conducted for the thermal elasti
c consolidation of a one-dimensional sand column made previously by Abousti
t. The practical analysis for the soil foundation demonstrated that the fre
ezing and thawing have not only related to the temperature variation, but a
lso related to the moisture migration. Reducing the permeability coefficien
t of the foundation soil, the freezing increases obviously due to the decre
asing of the pore water drainage. The freezing differences between the sand
-gravel pile and the silt-sand foundation due to the different heat conduct
ivity also illustrate that the fine-gravel layer can be a better measure to
resist the frozen heave in the road engineering in cold regions. (C) 2000
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