“…17,20 Sr complexes strongly with metal oxides (e.g. TiO2, FeOOH, Fe3O4) [21][22][23][24][25] through surface complexation reactions, and with clay minerals (e.g., talc, 17 illite, illite-smectite mixed layered phases, [25][26][27] bentonite, 28 and kaolinite 24,29 ) through both surface complexation and cation exchange reactions. 17,28,30 Cs interacts strongly with clay minerals through cation exchange reactions 17,26,31,32 and through surface complexation on the basal surface of clay minerals.…”