Equations of State for NaCl and CaCl2 Solutions of Arbitrary Concentration at Temperatures 423.15–623.15 K and Pressures up to 5 kbar
- Authors: Ivanov M.V.1, Bushmin S.A.1, Aranovich L.Y.2
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Affiliations:
- Institute of Precambrian Geology and Geochronology
- Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Issue: Vol 481, No 2 (2018)
- Pages: 1086-1090
- Section: Geochemistry
- URL: https://bakhtiniada.ru/1028-334X/article/view/193899
- DOI: https://doi.org/10.1134/S1028334X18080287
- ID: 193899
Cite item
Abstract
Equations of state valid for all possible salt concentrations in solution are obtained for binary fluids H2O—NaCl and H2O—CaCl2. The equations are based on the empirical form of the Gibbs free energy for salt solutions of arbitrary concentration, developed earlier. Based on experimental data on the PVTx properties the obtained earlier thermodynamic description of H2O—NaCl and H2O—CaCl2 solutions at saturated vapor pressure is extended towards higher pressures. For H2O—NaCl pressures are up to 5 kbar. For H2O—CaCl2 pressures cover the range of available experimental data up to 0.7 kbar. The equations allow precise calculation of the whole set of thermodynamic parameters of the discussed salt solutions in the temperature ranges 423.15–573.15 K and 423.15–623.15 K, corresponding to low temperature hydrothermal ore deposits, that could be relevant for thermodynamic modeling of ore-bearing fluids at such deposits.
About the authors
M. V. Ivanov
Institute of Precambrian Geology and Geochronology
Author for correspondence.
Email: m.v.ivanov@ipgg.ru
Russian Federation, Saint-Petersburg, 199034
S. A. Bushmin
Institute of Precambrian Geology and Geochronology
Email: m.v.ivanov@ipgg.ru
Russian Federation, Saint-Petersburg, 199034
L. Y. Aranovich
Institute of the Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: m.v.ivanov@ipgg.ru
Russian Federation, Moscow, 119017
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