Geochemistry of arsenic in low sulfide-high carbonate coal waste rock, Elk Valley, British Columbia, Canada
文摘
Geochemistry of As in low sulfide-high carbonate coal waste rock is discussed. The major As-containing mineral phases are primary pyrite and secondary Fe oxides. Carbonate dissolution facilitates Fe oxide precipitation during pyrite oxidation. Sorption to Fe oxides is a geochemical control on As release during pyrite oxidation. Fe oxides are a long-term sink for As in waste rock dumps under oxic conditions.