A set of perfect constitutive equations including the coupling effects of h
eat transfer and moisture migration is constructed for freezing soil, after
analyzing its thermomechanic properties, in the framework of continuum mec
hanics and mixture theory. By applying the theory, the influence of void ra
tio on frost heaving is studied after proposing a criterion for formation o
f layered ice; the results obtained coincide with experimental data availab
le in the literature. The temperature distribution of freezing soil is anal
yzed, the controlling equation deduced appears to be a nonlinear Burgers ty
pe equation with varying boundaries, which presents a theoretic foundation
for studying the nonlinear effects of heat-moisture migration in the freezi
ng process.