Abstract

The volumetric response of compacted bentonites against environmental actions is a key aspect in most designs of nuclear waste repositories. The safety assessment of such repositories must account for robust and reliable models of stress–strain for bentonites. While many models for unsaturated low activity clays take advantage from the use of a generalized effective stress, its application to expansive soils has not found the same degree of success. One of the possible reasons is the complex water retention behaviour of these materials, which only recently has been successfully reproduced by numerical models. Here, by adopting an appropriate water retention model, a coupled hydro-mechanical approach to simulate the volume change behaviour of compacted bentonites is suggested. An explicit distinction between interlayer adsorbed water and capillary water is used to simulate the water retention behaviour. It is then shown that by using a precise water retention formulation, the volumetric behaviour can be interpreted within an effective stress–degree of saturation based framework. Some interesting results derived from the use of the effective stress include the shrinkage limit, the increase in stiffness of the elastic regime and the use of a single elastic coefficient for both wetting–swelling and reloading stress paths.

Highlights

  • It is widely accepted that two constitutive stress variables are needed to model the mechanical behaviour of unsaturated soils [1]

  • While for low activity soils the interest of an effective stress considering the hydraulic state has been well recognized [3, 4], most models intended for expansive clays do not consider the hydraulic state (e.g. [5]), generally given by the water retention curve, (WRC) on the mechanical response under unsaturated states, even though solid-water interactions are the salient feature of this class of material

  • Bentonites can sustain high degrees of saturation at high suction values, a slight deviation of the simulated curve from reality can lead to a large deviation in the computed effective stress

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Summary

Introduction

It is widely accepted that two constitutive stress variables are needed to model the mechanical behaviour of unsaturated soils [1]. [5]), generally given by the water retention curve, (WRC) on the mechanical response under unsaturated states, even though solid-water interactions are the salient feature of this class of material. Bentonites can sustain high degrees of saturation at high suction values, a slight deviation of the simulated curve from reality can lead to a large deviation in the computed effective stress. In this paper an accurate WRC formulation is used to study the suitability of using a single mechanical stress to be used in constitutive modelling of compacted expansive clays.

Modelling water retention behaviour
Modelling volume change of bentonite
Calibration of the water retention model
Constitutive stress variables
Volume change model equations
Elastic response upon drying and wetting
Suction controlled oedometric tests
Conclusions
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