Thermodynamics of Arsenates, Selenites, and Sulphates in the Oxidation Zone of Sulfide Ores. XVI. Solubility of the Synthetic Analogue of Mandarinoite at 25°C

This study aims to synthesize two iron(III) selenites—Fe2(SeO3)3·5H2O (analogous to the mineral mandarinoite) and Fe2(SeO3)3·3H2O—and to investigate their solubility. The obtained samples were identified by powder X-ray diffraction and energy-dispersive X-ray microanalysis. Solubility was determined through the method of isothermal saturation at 25°C. To suppress the hydrolysis of Fe3+ ions and prevent the precipitation of iron hydroxide, the experiments were conducted in nitric- or sulfuric-acid solutions. The compositions of the saturated solutions were used to calculate the solubility product using a Geochemist’s Workbench (GMB 9.0, SpecE8 program). The calculated values of the solubility product are log Ksp(Fe2(SeO3)3·5H2O) = –38.6 ± 0.5 and log Ksp(Fe2(SeO3)3·3H2O) = –39.0 ± 0.2.

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Publication Details

Journal
Geology of Ore Deposits
Published
2024-12-01
DOI
https://doi.org/10.1134/s1075701524700314
Primary Topic
Crystal Structures and Properties
Type
article
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article

Thermodynamics of Arsenates, Selenites, and Sulphates in the Oxidation Zone of Sulfide Ores. XVI. Solubility of the Synthetic Analogue of Mandarinoite at 25°C

Astrid Holzheid, M. V. Charykova, В. Г. Кривовичев, N. V. Platonova et al.
Geology of Ore Deposits
Crystal Structures and Properties
article

Thermodynamics of Arsenates, Selenites, and Sulphates in the Oxidation Zone of Sulfide Ores. XVI. Solubility of the Synthetic Analogue of Mandarinoite at 25°C

Astrid Holzheid, M. V. Charykova, В. Г. Кривовичев, N. V. Platonova, K. L. Ushakova, N. M. Efimenko
article en

Abstract

This study aims to synthesize two iron(III) selenites—Fe2(SeO3)3·5H2O (analogous to the mineral mandarinoite) and Fe2(SeO3)3·3H2O—and to investigate their solubility. The obtained samples were identified by powder X-ray diffraction and energy-dispersive X-ray microanalysis. Solubility was determined through the method of isothermal saturation at 25°C. To suppress the hydrolysis of Fe3+ ions and prevent the precipitation of iron hydroxide, the experiments were conducted in nitric- or sulfuric-acid solutions. The compositions of the saturated solutions were used to calculate the solubility product using a Geochemist’s Workbench (GMB 9.0, SpecE8 program). The calculated values of the solubility product are log Ksp(Fe2(SeO3)3·5H2O) = –38.6 ± 0.5 and log Ksp(Fe2(SeO3)3·3H2O) = –39.0 ± 0.2.

Geology of Ore DepositsVol. 66(8)
St Petersburg University (RU), Christian-Albrechts-Universität zu Kiel (DE)
Clean water and sanitation
Openalex Percentile: Top 85%
Crystal Structures and Properties
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