Heterogeneous Swelling of an Isotropically Compacted Bentonite-Based Material

Experimental Observations and Modelling

Journal Article (2023)
Author(s)

Anne Catherine Dieudonné (TU Delft - Geo-engineering)

Claude Gatabin (Université Paris-Saclay, Paris)

Wissem Dridi (Université Paris-Saclay, Paris)

Jean Talandier (Agence nationale pour la gestion des déchets radioactifs)

Frederic Collin (Université de Liège)

Robert Charlier (Université de Liège)

Geo-engineering
Copyright
© 2023 A.A.M. Dieudonné, Claude Gatabin, Wissem Dridi, Jean Talandier, Frédéric Collin, Robert Charlier
DOI related publication
https://doi.org/10.1007/s00603-023-03476-z
More Info
expand_more
Publication Year
2023
Language
English
Copyright
© 2023 A.A.M. Dieudonné, Claude Gatabin, Wissem Dridi, Jean Talandier, Frédéric Collin, Robert Charlier
Geo-engineering
Issue number
6
Volume number
57
Pages (from-to)
4159-4172
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

This paper presents a comprehensive investigation of the swelling behaviour of a compacted bentonite–sand mixture subjected to hydration under constant volume conditions. Contrary to previous studies, the tested sample was isotropically compacted before being hydrated under constant volume conditions until full saturation was reached. The total axial pressure, total radial pressures at four different heights of the sample, and injected water volume were recorded over time. The experimental data reveal a complex and non-uniform evolution of the axial and radial stresses over time, as well as anisotropy of the total stresses, which persist at the saturated equilibrated state. To gain further insights, a numerical analysis was performed using an advanced hydromechanical framework for partially saturated porous media, accounting for the evolving microstructure of the material. The complex evolution of the total axial and radial pressures with time is attributed to the advancing hydration and swelling front in the sample, along with the development of irreversible strains. The good agreement between the numerical results and the experimental data enables validation of the developed framework. Implications for engineered barriers in deep geological disposal of radioactive waste are discussed.