Experimental and modelling study of the interaction of bentonite with alkaline water
Creators
- 1. Amphos 21 Consulting S.L., Calle Venecuela, 103, Barcelona 08019 (Spain)
- 2. CEA, DES, IRESNE, DEC, Cadarache, Saint-Paul-lez-Durance F-13108 (France)
- 3. Universite Paris-Saclay, CEA, Service d'Etude du Comportement des Radionucleides, Gif-Sur-Yvette 91191 (France)
- 4. BRGM Bureau de Recherches Geologiques et Minieres, Orleans (France)
- 5. Andra, Scientific and Technical Division, 1-7 Rue Jean Monnet, Chatenay-Malabry F-92298 (France)
Description
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. (authors)
Availability note (English)
Available from doi: https://doi.org/10.1016/j.clay.2023.107157Additional details
Identifiers
Publishing Information
- Journal Title
- Applied Clay Science
- Journal Issue
- v.246
- Journal Page Range
- p. 1-14
- ISSN
- 0169-1317
Conference
- Title
- 8. International Conference on Clays in Natural and Engineered Barriers for Radioactive Waste Confinement
- Dates
- 13-16 Jun 2022
- Place
- Nancy (France)
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- France
- INIS RN
- 55080382
- Subject category
- S12: MANAGEMENT OF RADIOACTIVE WASTES, AND NON-RADIOACTIVE WASTES FROM NUCLEAR FACILITIES;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- BENTONITE; CONCRETES; DISSOLUTION; HYDRATION; MONTMORILLONITE; POTASSIUM; POTASSIUM HYDROXIDES; RADIOACTIVE WASTES; SWELLING; UNDERGROUND; WATER
- Descriptors DEC
- ALKALI METAL COMPOUNDS; ALKALI METALS; BUILDING MATERIALS; CLAYS; DEFORMATION; ELEMENTS; HYDROGEN COMPOUNDS; HYDROXIDES; INORGANIC ION EXCHANGERS; ION EXCHANGE MATERIALS; LEVELS; MATERIALS; METALS; MINERALS; OXYGEN COMPOUNDS; POTASSIUM COMPOUNDS; RADIOACTIVE MATERIALS; SILICATE MINERALS; SOLVATION; WASTES
Optional Information
- Notes
- 67 refs.; Available from the INIS Liaison Officer for France, see the INIS website for current contact and E-mail addresses; This record replaces 55069299