Influence of Sulfur Content in Tailings on Processes of Hypergene and Technogene Mineral Formation on the Example of Kavalerovo Tin-Ore District

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The paper presents the results of the physicochemical modeling obtained with the use of the “Selektor” program of calculation of chemical equilibriums. We have determined the stability fields of hypergene and technogene minerals crystallized in the mining wastes (tailings) from the highly concentrated pore solutions forming the drainage waters of Kavalerovo district. Our investigations allowed us to obtained new data on the pH range of the hypergene and technogene mineral formation depending of the sulfur amount in the wastes coming with the flotation reagents and sulfides under conditions of the atmosphere influence and without it. This problem for the mining technogene system of the district under consideration is first proposed to be solved with the help of the method of the physicochemical modeling.

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605-609

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October 2014

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© 2014 Trans Tech Publications Ltd. All Rights Reserved

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[1] W.M. Clark, В. Cohen, An analysis of the theoretical relations between reduction potentials and рН, Public Health Reports, Reprint, 826 (1923), 666-683.

Google Scholar

[2] V.V. Sherbina, Redox potentials applied to the study of mineral paragenesis, Dokl. USSR Academy of Sciences, 22-8 (1939), 508-511.

Google Scholar

[3] C.E. Zоbe11, Studies on redox potentials of marine sediments, Bull. Am. Assoc. Petrol. Geol., 30 (1946), 477-513.

Google Scholar

[4] R.L. Starkey K.M. Wight, Anaerobic Corrosion of Iron in Soil, American Gas Association, New York, (1945).

Google Scholar

[5] В. Masоn, Oxidation and reduction in geochemistry, Journ. Geol, 57 (1949), 62-72.

Google Scholar

[6] M.J.N. Pourbaix, Thermodynamics of Dulite Aqueous Solutions, Edwar Arnold and Co., London, (1949).

Google Scholar

[7] R. Garrels, C. Christ, Solutions, minerals, equilibrium, Academic Press, New York, (1968).

Google Scholar

[8] I.K. Karpov, Physicochemical modeling with computer in geochemistry, Nauka, Novosibirsk, (1981).

Google Scholar

[9] N.N. Akinfiev, Physicochemical basis of modeling of hydrothermal systems, Doctoral thesis, Moscow, (1995).

Google Scholar

[10] D.N. Salikhov, G.I. Belikova, E.V. Sergeeva. Thermodynamics of equilibria of manganese ore minerals, Geological compilation IG USC RAS, 2 (2001), 163-167.

Google Scholar

[11] A.P. Boyarkin, Conditions of formation of magnesite and siderite deposits in the South Urals and forecasting, Candidate's thesis, Ufa, (1980).

Google Scholar

[12] A.M. Kostina, V.P. Zvereva. Hypergene Mineral Formation in the Tailing Dumps of Komsomolsky Tin-ore Area Depending on the Concentration of Sulfur in the Solution, Proceedings of the 2013 International Conference on Material Science and Environmental Engineering, Wuhan, China (2013).

DOI: 10.4028/www.scientific.net/amr.989-994.1297

Google Scholar

[13] A.M. Kostina, Estimation of the environmental situation of the mining technogenic system of tin-sulfide ore deposits of Komsomolsky region of the Far East using the physicochemical modeling, Candidate's thesis, Vladivostok, (2012).

Google Scholar

[14] S.I. Polkin, S.F. Laptev, Extraction of tin ores and alluvial deposits, Nauka, Moscow, (1974).

Google Scholar

[15] V.P. Zvereva, Environmental effects of hypergene processes in the tin-ore deposits of the Far East, Dalnauka, Vladivostok, (2008).

Google Scholar

[16] L.K. Yakhontova, V.P. Zvereva, Mineralogy of hypergene zone, Ref. allowance, Dalnauka, Vladivostok, (2007).

Google Scholar