Thermo-mechanical constitutive modeling of unsaturated clays based on the critical state concepts

• Published in: Journal of Rock Mechanics and Geotechnical Engineering Vol. 7; no. 2; pp. 193 - 198
• Main Authors: Saeed Tourchi, Amir Hamidi
• Format: Journal Article
• Language: English
• Published: Elsevier 01-04-2015
• Subjects: Cam-clay; Constitutive model; Critical state; Plasticity; Unsaturated clays
• ISSN: 1674-7755
• DOI: 10.1016/j.jrmge.2015.02.004

A thermo-mechanical constitutive model for unsaturated clays is constructed based on the existing model for saturated clays originally proposed by the authors. The saturated clays model was formulated in the framework of critical state soil mechanics and modified Cam-clay model. The existing model has been generalized to simulate the experimentally observed behavior of unsaturated clays by introducing Bishop's stress and suction as independent stress parameters and modifying the hardening rule and yield criterion to take into account the role of suction. Also, according to previous studies, an increase in temperature causes a reduction in specific volume. A reduction in suction (wetting) for a given confining stress may induce an irreversible volumetric compression (collapse). Thus an increase in suction (drying) raises a specific volume i.e. the movement of normal consolidation line (NCL) to higher values of void ratio. However, some experimental data confirm the assumption that this reduction is dependent on the stress level of soil element. A generalized approach considering the effect of stress level on the magnitude of clays thermal dependency in compression plane is proposed in this study. The number of modeling parameters is kept to a minimum, and they all have clear physical interpretations, to facilitate the usefulness of model for practical applications. A step-by-step procedure used for parameter calibration is also described. The model is finally evaluated using a comprehensive set of experimental data for the thermo-mechanical behavior of unsaturated soils.