A natural attenuation of arsenic in drainage from an abandoned arsenic mine dump |
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| Institution: | 1. Environmental Geochemistry, Bayreuth Center for Ecology and Environmental Research (BayCEER), University of Bayreuth, D-95440 Bayreuth, Germany;2. Department of Earth Sciences & Research Center on Natural Resources, Health and the Environment (RENSMA), University of Huelva, Huelva 21071, Spain;1. Mitsubishi Materials Corporation, 1-297 Kitabukuro, Omiya, Saitama 330-0835, Japan;2. Mitsubishi Materials Techno Corporation, 1-14-16 Kudankita, Chiyoda-ku, Tokyo 102-8205, Japan;3. Faculty of Systems Engineering, Wakayama University, 930 Sakaedani, Wakayama 113-0033, Japan;4. Japan Oil, Gas and Metals National Corporation, 2-10-1 Toranomon, Tokyo 105-0001, Japan;5. Graduate School Division of Science and Engineering, University of Toyama, 3190 Gofuku, Toyama 930-8555, Japan;1. Natural History Museum, Cromwell Road, London SW7 5BD, UK;2. Department of Earth Sciences, University of Huelva, 21071 Huelva, Spain |
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| Abstract: | At the abandoned As mine in Nishinomaki, Japan, discharged water from the mining and waste dump area is acidic and rich in As. However, the As concentration in the drainage has been decreased to below the maximum contaminant level (0.01 mg/l for drinking water, Japan) without any artificial treatments before mixing with a tributary to populated areas. This implies that the As concentration in water from the waste dump area has been naturally attenuated. To elucidate the reaction mechanisms of the natural attenuation, analysis of water quality and characterization of the precipitates from the stream floor were performed by measuring pH, ORP and electric conductivity on-site, as well as X-ray diffraction, ICP-mass spectrometry and ion-chromatography. Selective extractions and mineral alteration experiments were also conducted to estimate the distribution of As in constituent phases of the precipitates and to understand the stability of As-bearing phases, respectively. The water contamination resulted from oxidation of sulfide minerals in the waste rocks, i.e., the oxidation of pyrite and realgar and subsequent release of Fe, SO4, As(V) and proton. The released Fe(II) transformed to Fe(III) by bacterial oxidation; schwertmannite then formed immediately. While the As concentrations in the stream were lowered nearly to background level downstream, those in the ochreous precipitates were up to several tens of mg/g. The As(V) was effectively removed by the formed schwertmannite and had been naturally attenuated. Although schwertmannite is metastable with respect to goethite, the experiments show that the transformation of schwertmannite to goethite may be retarded by the presence of absorbed As(V) in the structure. Therefore, the attenuation of As in the drainage and the retention of As by schwertmannite are expected to be maintained for the long term. |
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