THERMODYNAMIC PROPERTIES OF UVAROVITE GARNET (CA3CR 2SI3O12)

dc.contributor.author	Klemme S.
dc.contributor.author	van Miltenburg J.C.
dc.contributor.author	Javorsky P.
dc.contributor.author	Wastin F.
dc.date.accessioned	2023-11-26T02:22:35Z
dc.date.available	2023-11-26T02:22:35Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=14525342
dc.identifier.citation	American Mineralogist, 2005, 90, 4, 663-666
dc.identifier.issn	0003-004X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/41966
dc.description.abstract	The low-temperature heat capacity of uvarovite (Ca3Cr2Si3O12) was measured between 2 and 400 K, and thermochernical functions were derived from the results. The measured heat-capacity curve shows a significant lambda-shaped anomaly peaking at around 9 K. The nature of this transition is unknown. From our data, we suggest a standard entropy for uvarovite at 298.15 K of 320.9 +/- 0.6 J/(mol(.)K).
dc.title	THERMODYNAMIC PROPERTIES OF UVAROVITE GARNET (CA3CR 2SI3O12)
dc.type	Статья
dc.identifier.doi	10.2138/am.2005.1812

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