“…On a spatial basis, lithological degeneration is the dominant factor in determining the total concentration of heavy metals in world soils. Sediments derived from formations composed of black shales, coals, limestones, ultramafic rocks and sedimentary ironstones are regularly enriched in several heavy metals, although content can vary (Alloway, 2013; Table 1). During weathering, these deposits undergo dissolution and oxidation, and metals are dispersed in regional soils, transported long distances via Aeolian or fluvial transport and/or leached into groundwater (Alloway, 2013;Sweet et al, 1989;Roen, 1984;Tuttle et al, 2009).…”