Atmospheric exposure of iron sulphide minerals, such as pyrite (FeS2) and arsenopyrite (FeAsS), around mine dumps and waste piles releases large amounts of SO4 2− and Fe2+ into nearby aquatic environments, such as streams and water channels. This leads to severe acidification of the affected water bodies, with pH levels as low as 1.0. Such acidity is a major global concern because it causes the dissolution of nearly all mineral phases. In addition to iron sulphides, similar acidic conditions can develop around other sulphide mines, such as those containing lead (PbS), zinc (ZnS), copper (CuS), and nickel (NiS). Toxic metals, including As, Pb, Cd, Zn, Cu, and Ni, are mobilized due to the dissolution of gangue materials in these extremely acidic environments, resulting in their enrichment in the surrounding ecosystem.