Abstract

Significant chemical influence on the swelling potential of MX-80 bentonite was observed during swelling tests where specimens were hydrated with highly concentrated brine. The maximum swelling pressure for specimens hydrated with brine was about 30% of the maximum swelling pressure for the same specimens hydrated with de-ionized water. The maximum swelling pressure was attained within tens of hours of brine infiltration and further decreased by half within a year. A fully coupled hydro–mechanical–chemical (HMC) dual-porosity model is proposed in this paper to interpret the swelling behaviour of MX-80 when infiltrated with brine. The dependence of hydraulic and mechanical properties on such factors as porosity, salinity and water content was investigated. A nonlinear elastic constitutive model was proposed to correlate the swelling pressure with the variation in the microporosity. The chemical effects on the mechanical behaviour were coupled at the micropore level. A number of relationships have been developed for MX-80, i.e. micropore permeability as a function of void ratio, water retention characteristics of micropores and macropores, micropore dependence on water content and the diffusion coefficients of the two types of pore structure. The proposed model was successful in reproducing both quantitatively and qualitatively the experimental results from two sets of infiltration experiments on compacted MX-80 bentonite.

Highlights

  • Bentonite has been widely considered as seal materials in nuclear waste disposal facilities [1, 13, 15, 43, 44, 53]

  • The maximum swelling pressure for specimens hydrated with brine was about 30% of the maximum swelling pressure for the same specimens hydrated with de-ionized water

  • The results showed that the swelling pressure of MX-80 bentonite hydrated with DI water reached a plateau in a monotonous manner after approximately 1 month

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Summary

Introduction

Bentonite has been widely considered as seal materials in nuclear waste disposal facilities [1, 13, 15, 43, 44, 53]. In order to interpret the observed chemical effects on the swelling behaviour of bentonite, the authors have developed in this paper a fully coupled HMC model that takes into account the dual-porosity structure of the bentonite. A HMC-coupled dual-porosity model was developed by Musso et al [34] to address the volume change of expansive soil under cycling of chemical permeation. This approach, only addressing the fully saturated situation, provides an excellent framework to interpret the chemical influences on the swelling behaviour of bentonite [8]. This paper is structured as follows: (1) characterization of hydraulic and transport properties of bentonite; (2) derivation of governing HMC equations; (3) development of finite element (FE) models; and (4) mathematical simulation of swelling tests

Double-porosity in bentonite
Hydraulic conductivity of a dual-porosity medium infiltrated with brine
M NaCl
Chemical transport properties: tortuosity and diffusion
WRC for MX-80 bentonite
Macropore WRC
Micropore WRC
Swelling pressure at various dry densities and salinities
HMC-coupled model for MX-80 bentonite
Hydraulic flow equations
Dual-porosity flow equations
Solute transport equations
Constitutive relationship for mechanical behaviour
1.10 Finite element model for constant volume swelling test
1.11 Simulation of Posiva test
1.12.1 Experimental results of temporal variation of swelling pressure
1.12.2 Modelled temporal variation of swelling pressure
Findings
Conclusion
Full Text
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