Thermodynamics of arsenates, selenites, and sulfates in the oxidation zone of sulfide ores. IX. Physicochemical formation conditions and thermal stability of zinc selenites
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  • 作者:M. V. Charykova ; E. L. Fokina ; E. V. Klimova ; V. G. Krivovichev…
  • 刊名:Geology of Ore Deposits
  • 出版年:2014
  • 出版时间:December 2014
  • 年:2014
  • 卷:56
  • 期:7
  • 页码:546-552
  • 全文大小:578 KB
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    5. Fokina, E.L., Klimova, E.V., Charykova, M.V., et al., Thermodynamics of arsenates, selenites, and sulfates in the oxidation zone of sulfide ores: VIII. Field of thermal stability of synthetic analog of chalcomenite and its dehydration and dissociation, / Geol. Ore Deposits, 2014, vol. 56, spec. issue 7 (Zapiski of the Russian Mineralogical Society), pp.
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    8. Krivovichev, V.G., Charykova, M.V., Yakovenko, O.S., and Depmeier, W., Thermodynamics of arsenates, selenites, and sulfates in the oxidation zone of sulfide ores: IV. Eh-pH diagrams of the Me-Se-H2O systems (Me = Co, Ni, Fe, Cu, Zn, Pb) at 25°C, / Geol. Ore Deposits, 2011, vol. 53, spec. issue 7 (Zapiski of the Russian Mineralogical Society), pp. 514-27. CrossRef
    9. Krivovichev, S.V. and Filatov, S.K., / Kristallokhimiya mineralov i neorganicheskikh soedinenii s kompleksami anionotsentrirovannykh tetraedrov (Crystal Chemistry of Minerals and Inorganic Compounds with Anion-Centered Tetrahedra), St. Petersburg: St. Petersburg State Univ., 2001.
    10. Krivovichev, V.G., Tarasevich, D.A., Charykova, M.V., et al., Thermodynamics of arsenates, selenites, and sulfates in the oxidation zone of sulfide ores: V. Chalcomenite and its synthetic analog, properties, and formation conditions, / Geol. Ore Deposits, 2012, vol. 54, spec. issue 7 (Zapiski of the Russian Mineralogical Society), pp. 498-02. CrossRef
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  • 刊物主题:Mineral Resources;
  • 出版者:Springer US
  • ISSN:1555-6476
文摘
The aim of this study is to create a physicochemical analysis of the formation conditions of synthetic zinc selenite, ZnSeO3 · 2H2O and an experimental investigation of its thermal stability, dehydration, and dissociation. This study has been carried out using a comprehensive thermal analysis (thermogravimetry and differential scanning calorimetry) within the temperature interval from 25-00°C. It has been established that ZnSeO3 · 2H2O dehydrates at 81-22°C through four stages corresponding to the formation of intermediate hydrate species: ZnSeO3 · 5/3H2O, ZnSeO3 · H2O, and ZnSeO3 · 1/3H2O. It is suggested that under natural oxidation conditions zinc selenite precipitates as stable (ZnSeO3 · 2H2O) or metastable (ZnSeO3 · H2O) species. Anhydrous ZnSeO3 presumably exists at a higher temperature (up to 479°C) and breaks down within a temperature interval of 479-97°C to form ZnO and SeO2.

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