This paper describes experimental and numerical approaches to account for the effect of temperature on the residual shear strength of soil under slow-to-rapid shearing rates. We used ring-shear test results obtained on reconstituted samples of Ca-Mg bentonite, which were sheared to evaluate the drained residual friction angle ( ) under various confining stresses ( ), shearing rates ( ), and temperatures ( ). These results highlighted a dependence of on both and . In particular, thermal strengthening was observed under relatively low , which turned into thermal weakening under high . To reproduce this behaviour, we propose a non-isothermal viscoplastic model, which we implemented in a finite-element computer code for thermo-hydro-mechanical analysis of porous media. We calibrated the model using the experimental results, achieving a satisfactory performance. Owing to the significance of thermal effects in soil, we argue that approaches such as ours should be developed further and incorporated in modelling practices.
10th European Conference on Numerical Methods in Geotechnical Engineering (NUMGE2023)
7. Dams, embankments and slopes