Presents a fully coupled numerical model to simulate the slow transien
t phenomena involving heat and mass transfer in deforming partially sa
turated porous materials. Makes use of the modified effective stress c
oncept together with the capillary pressure relationship. Examines pha
se changes (evaporation-condensation), heat transfer through conductio
n and convection, as well as latent heat transfer. The governing equat
ions in terms of gas pressure, capillary pressure, temperature and dis
placements are coupled non-linear differential equations and are discr
etized by the finite element method in space and by finite differences
in the time domain. The model is further validated with respect to a
documented experiment on partially saturated soil behaviour, and the e
ffects of two-phase flow, as compared to the one-phase flow solution,
are analysed. Two other examples involving drying of a concrete wall a
nd thermoelastic consolidation of partially saturated clay demonstrate
the importance of proper physical modelling and of appropriate choice
of the boundary conditions.