Abstract
Coal samples from high arsenic coal areas have been analyzed by electron micropbe analyzer (EMPA), scanning electron microscopy with an energy dispersive X-ray analyzer (SEM-EDX), X-ray diffinction analysis (XRD), low temperature ashing (LTA), transmission electron microscopy (TEM), X-ray absorption fine structure (XAFS), instnunent neutron activation analysis (INAA) and wet chemical analysis. Although some As-bearing minerals such as pyrite, arsenopyrite, realgar (?), As-bearing sulfate, and As-bearing clays are found in the high arsenic coals, their contents do not account for the abundance of arsenic in the some coals. Analysis of the coal indicates that arsenic exists mainly in the form of As 5+ and As 3+, combined with compounds in the organic matrix. The occurrence of such exceptionally high arsenic contents in coal and the fact that the arsenic is dominantly organically associated are unique observations. The modes of occurrence of arsenic in high As-coals are discussed.
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References
North, D. W., Gibb, H. J., Abernathy, C. O., Arsenic: past, present and future considerations, inArsenic: Exposure and Health Effects (eds. Abemathy, C., Calderon, 0. R. L., Chappell, W. R.), New York: Chapman Hall, 1997, 406–423.
WHO,Environmental Health Criteria 18,Arsenic, Geneva, 1981, 118.
Zheng Baoshan, Wang Huadong, Geochemistry of arsenic, inEndemic Arsenism and Black-Foot Disease (ed. Wang, L. F.) (in Chinese), Urumqi: Xinjiang Science-tech Sanitation Publishing House, 1997, 13–33.
Zheng Baoshan, Zhang, J., Ding, Z. H. et al., Issues of health and disease relating to coal use in Southwest Guizhou Province,International Journal of Coal Geology, 1999, 40: 119.
Zhao Fenghua, Ren Deyi, Zheng Baoshan et al., Study on EXAFS of arsenic occurrence in high As-bearing coals,Chinese Sciences BuWetin, 1998, 43: 1549.
Belkin, H. E., Zheng, B., Finkelman, R. B., Geochemistry of coals causing arsenism in southwest China,U. S. Geological Swvey Open File Report 97–496, 4thInternational Symposium on Environmental Geochemistry, 10.
Finkelman, R. B., Modes of occurrences of trace elements in coals, USGS,Open File Report, 1981, OFR-81-99.
Bouska, V.Geochemistry of Coal, Prague: Academia, 1981, 165.
Coleman, S. L, Bragg L. J., Distribution and mode of occurrence of arsenic in coal,Recent Advances in Coal Geochemistry,Special Paper of the Geological Society of American, 1990, 13.
Huggins, F. E., Huffman, G. P.,Application of XAFS Spectroscopy to Coal Geochemistry, Mineral Spectroscopy:A Tribute to Roger G. Burns, The Geochemical Society, Special Publication 5th (eds. Dyar, MD., McCmunon, C., Schaefer, MW.), 133–51.
National Standard of the People’ s Republic of China (GB 3058–82):Detennimtion of Arsenic in Coal (in Chinese), Beijing: Technology Standard Publishing House, 1982.
Swaine, D. J.,Traee Elements in Coal London: Butterworths, 1990.
Bragg, L. J., Oman, J. K., Tewalt, S.J. et al., U. S. Geological Survey Coal Quality Database,U.S. Geological Survey Open File Report, 1997, 97.
Wang Pu, Pan Zhaolu, Weng Lingbao,System Mineralogy (in Chinese) (I), Beijing: Geological Publishing House, 1984, 342.
Palmer, C. A., Krasnow, M. R., Finkelman, R. B. et al., An evaluation of leaching to determine modes of occurrence of selected toxic elements in coal,J. Coal Quality, 1993, 12: 135.
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Project supported by the National Natural Science Foundation of China (Grant Nos. 49273189, 49873007), Key Roject of the Chinese Academy of Sciences, the Education Foundation of Sir Wang Kuan-Cheng (Hong Kong), and the Venture Capitol Foundation (U.S.Geological Survey).
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Ding, Z., Zheng, B., Zhang, J. et al. Preliminary study on the mode of occurrence of arsenic in high arsenic coals from southwest Guizhou Province. Sci. China Ser. D-Earth Sci. 42, 655–661 (1999). https://doi.org/10.1007/BF02877793
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DOI: https://doi.org/10.1007/BF02877793