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The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C. / Charykova, M.V.; Krivovichev, V.G.; Ivanova, N.M.; Semenova, V.V.

In: Geology of Ore Deposits, Vol. 57, No. 8, 2015, p. 691-698.

Research output: Contribution to journal › Article › peer-review

Harvard

Charykova, MV, Krivovichev, VG, Ivanova, NM & Semenova, VV 2015, 'The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C', Geology of Ore Deposits, vol. 57, no. 8, pp. 691-698. https://doi.org/10.1134/S1075701515080036, https://doi.org/10.1134/S1075701515080036

APA

Charykova, M. V., Krivovichev, V. G., Ivanova, N. M., & Semenova, V. V. (2015). The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C. Geology of Ore Deposits, 57(8), 691-698. https://doi.org/10.1134/S1075701515080036, https://doi.org/10.1134/S1075701515080036

Vancouver

Charykova MV, Krivovichev VG, Ivanova NM, Semenova VV. The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C. Geology of Ore Deposits. 2015;57(8):691-698. https://doi.org/10.1134/S1075701515080036, https://doi.org/10.1134/S1075701515080036

Author

Charykova, M.V. ; Krivovichev, V.G. ; Ivanova, N.M. ; Semenova, V.V. / The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C. In: Geology of Ore Deposits. 2015 ; Vol. 57, No. 8. pp. 691-698.

BibTeX

@article{3f7a1570001e482ba0f7e8e30d6d7d9f,
title = "The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C",
abstract = "The aim of this study is the synthesis of CuSeO3 center dot 2H(2)O (chalcomenite analog), ZnSeO3 center dot 2H(2)O, and ZnSeO3 center dot H2O and the investigation of their solubility in water. CuSeO3 center dot 2H(2)O has been synthesized from solutions of Cu nitrate and Na selenite, while Zn selenites were synthesized from solutions of Zn nitrate and Na selenite. The samples obtained have been examined with X-ray diffraction and infrared and Raman spectroscopy. The solubility has been determined using the isothermal saturation method in ampoules at 25 degrees C. The solubility has been calculated using the Geochemist's Workbench (GMB 9.0) software package. Solubility products have been calculated for CuSeO3 center dot 2H(2)O (10(-10.63)), ZnSeO3 center dot 2H(2)O (10(-8.35)), and ZnSeO3 center dot H2O (10(-7.96)). The database used comprises thermodynamic characteristics of 46 elements, 47 base particles, 48 redox pairs, 551 particles in solution, and 624 solid phases. The Eh-pH diagrams of the Zn-Se-H2O an",
author = "M.V. Charykova and V.G. Krivovichev and N.M. Ivanova and V.V. Semenova",
year = "2015",
doi = "10.1134/S1075701515080036",
language = "English",
volume = "57",
pages = "691--698",
journal = "Geology of Ore Deposits",
issn = "1075-7015",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "8",

}

RIS

TY - JOUR

T1 - The Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores. XI. Solubility of Synthetic Chalcomenite Analog and Zinc Selenite at 25 degrees C

AU - Charykova, M.V.

AU - Krivovichev, V.G.

AU - Ivanova, N.M.

AU - Semenova, V.V.

PY - 2015

Y1 - 2015

N2 - The aim of this study is the synthesis of CuSeO3 center dot 2H(2)O (chalcomenite analog), ZnSeO3 center dot 2H(2)O, and ZnSeO3 center dot H2O and the investigation of their solubility in water. CuSeO3 center dot 2H(2)O has been synthesized from solutions of Cu nitrate and Na selenite, while Zn selenites were synthesized from solutions of Zn nitrate and Na selenite. The samples obtained have been examined with X-ray diffraction and infrared and Raman spectroscopy. The solubility has been determined using the isothermal saturation method in ampoules at 25 degrees C. The solubility has been calculated using the Geochemist's Workbench (GMB 9.0) software package. Solubility products have been calculated for CuSeO3 center dot 2H(2)O (10(-10.63)), ZnSeO3 center dot 2H(2)O (10(-8.35)), and ZnSeO3 center dot H2O (10(-7.96)). The database used comprises thermodynamic characteristics of 46 elements, 47 base particles, 48 redox pairs, 551 particles in solution, and 624 solid phases. The Eh-pH diagrams of the Zn-Se-H2O an

AB - The aim of this study is the synthesis of CuSeO3 center dot 2H(2)O (chalcomenite analog), ZnSeO3 center dot 2H(2)O, and ZnSeO3 center dot H2O and the investigation of their solubility in water. CuSeO3 center dot 2H(2)O has been synthesized from solutions of Cu nitrate and Na selenite, while Zn selenites were synthesized from solutions of Zn nitrate and Na selenite. The samples obtained have been examined with X-ray diffraction and infrared and Raman spectroscopy. The solubility has been determined using the isothermal saturation method in ampoules at 25 degrees C. The solubility has been calculated using the Geochemist's Workbench (GMB 9.0) software package. Solubility products have been calculated for CuSeO3 center dot 2H(2)O (10(-10.63)), ZnSeO3 center dot 2H(2)O (10(-8.35)), and ZnSeO3 center dot H2O (10(-7.96)). The database used comprises thermodynamic characteristics of 46 elements, 47 base particles, 48 redox pairs, 551 particles in solution, and 624 solid phases. The Eh-pH diagrams of the Zn-Se-H2O an

U2 - 10.1134/S1075701515080036

DO - 10.1134/S1075701515080036

M3 - Article

VL - 57

SP - 691

EP - 698

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 8

ER -

ID: 3955491