“…Chromium(III), the dominant form in most minerals, is only sparingly soluble in water and strongly sorbed in mineral surfaces (Nriagu and Nieboer, 1988;Kotas and Stasicka, 2000). In the presence of manganese oxides, chromium(III) is oxidized to chromium(VI) , which under oxic, alkaline conditions, can desorb from mineral surfaces and become soluble in groundwater as an oxyanion (Eary and Rai, 1987;Kotas and Stasicka, 2000;Izbicki and others, 2008). The concentration of chromium(VI) in groundwater from natural sources generally is greatest where the combination of all the following conditions exist: abundant, easily weathered chromium-bearing minerals; manganese oxides on surfaces of aquifer materials; oxic, alkaline groundwater; and long residence times others, 2008, 2015;Morrison and others, 2009;Mills and others, 2011).…”