“…[2][3][4] Precipitation and coprecipitation methods, which are based on the K sp theory, are widely applied for material preparation or ionic removal in fields of energy, environment, health, catalysis, sensing, and so on. [5][6][7][8][9][10] Furthermore, the K sp gap between two ionic compounds sharing the same cation or anion can trigger precipitation transformation reactions, which widely exist in nature and daily life. For instance, the deeper ores of sphalerite (ZnS, K sp = 1.6 × 10 −24 ) and galena (PbS, K sp = 8.0 × 10 −28 ) can be converted to covellite (CuS, K sp = 6.3 × 10 −36 ) after being infiltrated by CuSO 4 solution, which are formed by the oxidation and eluviation of the shallower primary copper sulfide ore.…”