“…For smectite, the one-site ion exchange model developed by Wanner et al (1996) was used. This one-site model can describe Cs + sorption in various types of smectite and bentonite, and solution conditions (Wanner et al, 1996;Ochs et al, 2001;Tachi et al, 2009a), although it has been confirmed that Cs + sorbs on smectite as inner-sphere and outer-sphere complexes by NMR (Kim et al, 1996b) and EXAFS (Bostick et al, 2002). Model parameters, including site types, site capacities, and equilibrium constants (K) of ion exchange reactions with Na + , K + and NH 4 + , taken directly from the above literature, were expressed by the following equations (Table 4):…”