“…These differences (in absolute values, and in the trend as a function of pH) suggest differences in the mechanisms of Cs interaction with illite-smectite at trace and at elevated concentrations. These different mechanisms depend on concentration and surface coverage and can include diffusion into the interlayer of illite-smectite 24,25,31,37,38 and complexation at the frayed edges sites 29,30,39 at trace concentrations, and outer sphere surface complexes, 24,[32][33][34] and complexation at the silicon vacancies on the basal surfaces 19,35 at elevated concentrations. Sr complexation with illite-smectite was significant, and show similar trends with varying pH values, at both trace and elevated Sr concentrations.…”