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Karl Schaettle1, Luis Ruiz Pestana2, Teresa Head-Gordon1
1Department of Chemical and Biomolecular Engineering, University of California, Berkeley, Berkeley, California 94720, USA.
Cesium-137 (Cs+) exchange in micaceous clays is modeled, revealing that neighboring Cs-exchanged layers expand K-illite interlayers. This structural relaxation favors ordered Cs- and K-illite interstratification over adjacent exchange.
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