This paper focuses on investigating how a particular but classical configuration of finite homogeneous soil layer, once studied by Terzaghi and currently subjected to freezing temperatures, behaves different boundary conditions can intervene affect the thermo-hydro-mechanical (THM) responses. Spatial homogeneity is strong assumption has decisive advantage simplicity, allowing eventually constru...

A coupling of a physically based model of snowmelt runoff generation with the Monte-Carlo simulation of the model inputs is applied. The model of runoff generation is based on the finiteelement schematization of river basin and includes the description of the following hydrological processes: snow cover formation and snowmelt, freezing and thawing of soil, vertical soil moisture transfer and in...