Abstract—
Pectolite H1.00Na0.96Ca2.00\({\text{Mn}}_{{0.02}}^{{2 + }}\)Si3.00O9 from nepheline−feldspathic veins in the Kovdor massif, Kola Peninsula, Russia, was studied by X-ray diffraction (XRD), IR and Raman spectrometry, microprobe analysis (EPMA), and thermal analysis. The enthalpy of formation of pectolite HNaCa2Si3O9.from elements ∆fH° (298.15 K) = –4651.0 ± 4.3 kJ/mol was determined by melt solution calorimetry on a Setaram Tian–Calvet (France) microcalorimeter. The enthalpy of formation of serandite HNaMn2Si3O9, the manganese end member of the pectolite–serandite isomorphic series, was determined to be ΔH(298.15 K) = −4052.6 ± 4.4 kJ/mol. The absolute entropies and Gibbs energies of pectolite and serandite were calculated.
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ACKNOWLEDGMENTS
The authors thank the administration of the Geological Faculty, Lomonosov Moscow State University, for making available for this study the STOE-STADI MP powder X-ray diffractometer, FSM-1201 FTIR spectrometer, EnSpectr R532 Raman microscope, Q-1500D derivatograph, and Setaram Tian–Calvet microcalorometer that are installed at the faculty.
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Translated by E. Kurdyukov
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Ogorodova, L.P., Gritsenko, Y.D., Vigasina, M.F. et al. Thermodynamic Properties of Pectolite. Geochem. Int. 61, 75–81 (2023). https://doi.org/10.1134/S0016702923010056
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DOI: https://doi.org/10.1134/S0016702923010056