Effect of groundwater chemistry on the swelling behavior of a Ca-bentonite for deep geological repository |
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Affiliation: | 1. Department of Engineering, Huzhou University, Huzhou 313000, PR China;2. School of Nuclear Science and Technology, University of South China, Hengyang 421001, PR China;3. Paul Scherrer Institute, Laboratory for Waste Management, CH-5232 Villigen PSI, Switzerland;1. AITEMIN, C/ Margarita Salas 14, Parque Leganés Tecnológico, 28918 Leganés, Madrid, Spain;2. CIEMAT, Avd. Complutense 40, 28040 Madrid, Spain;1. BGR, Bundesanstalt für Geowissenschaften und Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany;2. Ruhr University Bochum, RUB, Chair for Foundation Engineering, Soil and Rock Mechanics, Universitätsstraße 150, D-44780 Bochum, Germany;3. LBEG, Landesamt für Bergbau, Energie und Geologie, Stilleweg 2, D-30655 Hannover, Germany |
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Abstract: | The swelling properties of buffer material for high level radioactive waste repository in a near-field environment are of particular importance for achieving the low permeability sealing function. In this study, the free swelling behavior of a potential buffer material Zhisin clay is evaluated under simulated groundwater conditions such as immersion in NaCl, CaCl2, and Na2SO4 solutions at various concentrations. Experimental results indicate that Zhisin clay, being a Ca-bentonite, exhibits reduced swelling strain in salt solutions. The amount of decrease in swelling strain upon saline water intrusion is affected by both the type and concentration of electrolyte. At the same concentration, the swelling strains in CaCl2 solution are lower than those in NaCl solution due to the quasi-crystals formed in the presence of calcium ions. Also, the swells in Na2SO4 solution are found to be lower than those in NaCl solution. This is attributed to the precipitation of CaSO4, which acts as binding agent and results in aggregation of clay particles. |
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Keywords: | Bentonite Geological repository Swelling Groundwater chemistry |
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