“…One-fourth of the Si in the hexagonal mesh layer is replaced by Al, resulting in a residual charge in the structural layer, which requires cations such as K, Na, Rb, or Cs to enter into the structural layers for balancing the charge . On the one hand, during the weathering of natural mica minerals, interlayer ions may be replaced by Na + , Cu 2+ , and Mg 2+ to form sodium mica, copper-bearing mica, and vermiculite. − On the other hand, by controlling the modification conditions, the interlayer structure of mica can be pillared or intercalated by Al 3+ , Ni 2+ , Zr 4+ , Ti 4+ , and organic ammonium to prepare environmental materials with excellent adsorption or catalytic properties. ,− The above cases indicate that the interlayer ions of mica minerals are not adequately stable, and they could be replaced or exchanged with other cations by regulating the reaction conditions. Herein, those cases provide a feasible reference for ion exchange-enhanced leaching (IEEL) of Rb occurring in the interlayers of biotite.…”