THERMODYNAMIC PROPERTIES AND STABILITY OF ALF-BEARING TITANITE CATIOSIO4-CAALFSIO4

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dc.contributor.author Troitzsch U.
dc.contributor.author Ellis D.J.
dc.date.accessioned 2021-04-13T02:40:31Z
dc.date.available 2021-04-13T02:40:31Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=859449
dc.identifier.citation Contributions to Mineralogy and Petrology, 2002, 142, 5, 626
dc.identifier.issn 0010-7999
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27743
dc.description.abstract Calorimetric and experimental data on AlF-bearing titanite are presented that yield thermodynamic properties of CaAlFSiO4, as well as activity-composition relations of binary titanite CaTiOSiO4–CaAlFSiO4. The heat capacity of synthetic CaAlFSiO4 was measured with differential scanning calorimetry between 170 and 850 K: C P =689.96–0.38647T+2911300T –2–8356.1T –0.5+0.00016179T 2 . Based on low-temperature heat capacity calculations with lattice vibrational theory (Debye model), the calorimetric entropy of CaAlFSiO4 can be expected to lie between 104.7 and 118.1 J mol–1 K–1. The temperature of the P21/a to A2/a phase change was determined calorimetrically for a titanite with X Al=0.09 (Ttransition =390 K). The decrease of the transition temperature at a rate of about 11 K per mol% CaAlFSiO4 is in good agreement with previous TEM investigations. The displacement of the reaction anorthite + fluorite = CaAlFSiO4 in the presence of CaTiOSiO4 was studied with high P–T experiments. Titanite behaves as a non-ideal, symmetrical solid-solution. The thermodynamic properties of CaAlFSiO4 consistent with a multi-site mixing model.
dc.title THERMODYNAMIC PROPERTIES AND STABILITY OF ALF-BEARING TITANITE CATIOSIO4-CAALFSIO4
dc.type Статья


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