“…Since the reactivity of silicates and their effects on the general consumption of acid in leaching can become more complex than the carbonates themselves, as indicated [61], it is worth mentioning that some silicate and aluminosilicate minerals, such as mica and clay minerals, can consume acid generated by the oxidation phenomenon [62][63][64]. Minerals, such as montmorillonite, kaolinite, and smectite, can quickly adsorb acid [65,66].…”