Abstract—
Coquimbite Al\({\text{Fe}}_{3}^{{3 + }}\)[SO4]6(H2O)12⋅6H2O (sample from the Javier Mine, Peru) has been studied by thermal and electron microprobe analysis, X-ray powder diffraction, Raman spectroscopy, and Mössbauer spectroscopy. The enthalpy of formation of the coquimbite from elements ∆fH0(298.15 K) = −11 118 ± 40 kJ/mol was determined by the method of solution calorimetry in melt of lead borate 2PbO∙B2O3 on a Setaram (France) Calvet microcalorimeter. The value of its absolute entropy S0(298.15 K) = 1248.3 ± 3.0 J/(mol K) was estimated, the entropy of formation ∆fS0(298.15 K) = − 5714.0 ±3.0 J/mol K), and the Gibbs energy of formation from elements ∆fG0(298.15 K) = −9411 ± 40 kJ/mol were calculated. The values of the enthalpy and Gibbs energy of formation of aluminocoquimbite Al2\({\text{Fe}}_{2}^{{3 + }}\)[SO4]6(H2O)12⋅6H2O from elements were estimated at −11 540 ± 29 and −9830 ± 29 kJ/mol, respectively.
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The thermal equipment and mass spectrometer are installed at and belong to the Chemical Faculty of Lomonosov Moscow State University, and the diffractometer, scanning electron microscope, Raman microscope, and Calvet microcalorimeter are installed at and belong to the Geological Faculty of Lomonosov Moscow State University.
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Translated by E. Kurdyukov
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Gritsenko, Y.D., Ogorodova, L.P., Vigasina, M.F. et al. Thermodynamic Properties of Coquimbite and Aluminocoquimbite. Geochem. Int. 61, 643–649 (2023). https://doi.org/10.1134/S0016702923050051
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DOI: https://doi.org/10.1134/S0016702923050051