Abstract
Experimental data available in the literature on the solubility of Cu (met.) and Cu2O (cuprite) in water under hydrothermal conditions have been processed. Key experiments on the solubility of cuprite were carried out at 300°C and the saturated vapor pressure of H2O vs. pH of the solution. As a result, a set of values of thermodynamic properties for 25°C, 1 bar and the parameters of the Helgeson–Kirkham–Flowers and Akinfiev–Diamond equations of state for Cu(I) hydroxocomplexes were obtained, which make it possible to describe their behavior in a wide range of temperatures (0–600°C), pressures (1–3000 bar), and densities of aqueous fluid (0.01–1 g/cm3). As has been shown by thermodynamic modeling, Cu+ ions are prevalent in the acidic and weakly alkaline regions of the aqueous solvent over the entire temperature and pressure range studied. The effect of the neutral CuOH hydroxocomplex begins to show up in the alkaline region at T > 300°C and grows with increasing temperature. The second copper hydroxocomplex \({\text{Cu}}\left( {{\text{OH}}} \right)_{2}^{ - }\) shows up only in the strongly alkaline region, and the temperature has almost no effect on its behavior.
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ACKNOWLEDGMENTS
The authors are grateful to L.N. Var’yash for providing crystalline cuprite for the experiments and to S. Aksenov, who took part in the experimental work.
Funding
This work was supported by the Russian Science Foundation, grant no. 20-17-00184.
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Akinfiev, N.N., Zotov, A.V. Copper in Hydrothermal Systems: a Thermodynamic Description of Hydroxocomplexes. Geol. Ore Deposits 65, 1–10 (2023). https://doi.org/10.1134/S1075701523010026
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DOI: https://doi.org/10.1134/S1075701523010026