Experimental and modelling study of the interaction of bentonite with alkaline water

• Published in: Applied clay science 2023-12, Vol.245, p.107157, Article 107157
• Main Authors: Pelegrí, J., Laviña, M., Bernachy-Barbe, F., Imbert, C., Idiart, A., Gaboreau, S., Cochepin, B., Michau, N., Talandier, J.
• Format: Article
• Language: English
• Subjects: Chemo-mechanical couplings; Compacted bentonite; Earth Sciences; Experimental and modelling study; Interaction with KOH rich water; Sciences of the Universe; Swelling pressure
• ISSN: 0169-1317; 1872-9053
• DOI: 10.1016/j.clay.2023.107157

Compacted bentonite is planned to be used as buffer and backfill materials for the containment of radioactive waste in underground repositories. The performance of these barriers depends on the swelling capacity of bentonite upon hydration. Prolonged interaction between bentonite and alkaline fluids from neighbouring concrete structures can impair the swelling capacity due to profound changes in the chemical composition of bentonite. The coupled hydro-chemo-mechanical behaviour of bentonite under such conditions is at present not well understood. This paper presents for the first time a combined experimental and modelling study that addresses this coupled behaviour with the aim of understanding the key mechanisms leading to swelling pressure loss. Two experiments are presented in which compacted Wyoming bentonite was saturated with either clay or cementitious water, leading to different initial swelling capacities. The samples were subsequently subject to a flow of a KOH-rich cementitious water leading to a slow but sustained decrease in swelling pressure in both tests. The main novelty is the application of a recently developed hydro-chemo-mechanical model for bentonite for interpretation of the experiments. The model accounts for the impact of montmorillonite dissolution, cation exchange reactions, and changes in salinity on the swelling capacity of bentonite. The model results show a relatively good agreement with experimental measurements and suggest that the decrease in swelling capacity of bentonite is driven primarily by an increase in potassium fraction in the interlayer water and by montmorillonite dissolution. •Compacted Wyoming bentonite is saturated and percolated with cementitious (KOH rich) water.•Sustained decrease in the swelling pressure upon cementitious water injection.•Hydro-chemo-mechanical (HCM) model for swelling clays based on the Barcelona Basic Model (BBM).•Swelling pressure loss is dominated by K+ uptake in the interlayer.