“…Many minerals, including marble, hydrothermal veins, sulfide veins, and calcareous shales, naturally contain arsenic combined with sulfur and other metals 9 . So, it can be found in unused mineral excavation sites from the past, where soils and water sources have accumulated 10 . The aerial oxidation of pyrite material lowers the pH of the groundwater and facilitates the hydrolysis of ferric arsenate and ferric arsenite, which are the most common alternation products of arsenopyrite 11 .…”