STRUCTURE AND PHASE TRANSITION OF CAGE2O5 REVISITED

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dc.contributor.author Malcherek T.
dc.contributor.author Bosenick A.
dc.date.accessioned 2022-10-30T05:34:04Z
dc.date.available 2022-10-30T05:34:04Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=6470601
dc.identifier.citation Physics and Chemistry of Minerals, 2004, 31, 4, 224-231
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/39292
dc.description.abstract The structure of CaGe2O5 between room temperature and 923 K has been determined by X-ray powder diffraction. A continuous phase transition from triclinic C1¯ to monoclinic C2/c symmetry at Tc*=714±3 K is observed. The transition is accompanied by a weak heat capacity anomaly. This anomaly and the strain analysis based on the measured lattice parameters indicate a classical second-order phase transition. The order parameter, as measured by the strain component e23, is associated with the displacement of the Ca cation. Electronic structure optimization by density functional methods is used to verify the centric space group of the low-temperature structure of CaGe2O5.
dc.subject PHASE TRANSITION
dc.subject TITANITE
dc.subject SPHENE
dc.subject DISPLACIVE
dc.subject MICROSTRAIN
dc.title STRUCTURE AND PHASE TRANSITION OF CAGE2O5 REVISITED
dc.type Статья


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