A thermomechanical model for saturated clays is proposed within the framewo
rk of recent extensions of the Cam-Clay model. The results of some tests fo
und in the literature are analyzed, and the main features of the thermomech
anical behaviour of clays are identified. The effect of the overconsolidati
on ratio (OCR) on the volume change of a soil (expansion-contraction) submi
tted to heating is well established using experimental data obtained for se
lected soils by various authors. However, existing models need to be modifi
ed to correctly model this feature. For this reason, a new volumetric therm
al plastic mechanism is developed that allows for the prediction of plastic
strains at higher OCR values. The overconsolidation effect observed when h
eating a normally consolidated soil is also modelled. Particular attention
is paid to the coupling and hardening phenomena related to the combined eff
ects of stress and temperature. A qualitative validation is made by examini
ng the response of the model under a given thermomechanical path. Compariso
n with existing thermomechanical experimental results shows that the model
can provide satisfactory predictions.