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Pressure and temperature-dependent Raman study of YLiF4

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dc.contributor.author Sarantopoulou, E en
dc.contributor.author Raptis, YS en
dc.contributor.author Zouboulis, E en
dc.contributor.author Raptis, C en
dc.date.accessioned 2014-03-01T01:15:04Z
dc.date.available 2014-03-01T01:15:04Z
dc.date.issued 1999 en
dc.identifier.issn 0163-1829 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/13326
dc.subject Temperature Dependence en
dc.subject.classification Physics, Condensed Matter en
dc.subject.other FLUORIDE SCHEELITES en
dc.subject.other LATTICE-VIBRATIONS en
dc.subject.other LIYF4 en
dc.subject.other ND en
dc.subject.other SPECTROSCOPY en
dc.subject.other SCATTERING en
dc.subject.other ABSORPTION en
dc.subject.other CONSTANTS en
dc.subject.other DYNAMICS en
dc.subject.other YLF en
dc.title Pressure and temperature-dependent Raman study of YLiF4 en
heal.type journalArticle en
heal.identifier.primary 10.1103/PhysRevB.59.4154 en
heal.identifier.secondary http://dx.doi.org/10.1103/PhysRevB.59.4154 en
heal.language English en
heal.publicationDate 1999 en
heal.abstract Raman scattering spectra of single crystals of YLiF4 have been measured over wide ranges of hydrostatic pressures (0-20 GPa) and temperatures (30-1000 K). Unlike other members of the scheelite crystal class, the internal modes of YLiF4 due to vibrations within the LiF4-3 tetrahedra display large partial derivative omega/partial derivative P and partial derivative omega/partial derivative T slopes. In contrast, all four external modes corresponding to lattice translations show small partial derivative omega/partial derivative P slopes, with one of them (whose observation from the pressure cell is clear) also showing a small partial derivative omega/partial derivative P slope. These results suggest that temperature or pressure affect primarily the dynamics of the LiF4-3 group. This conclusion is further supported by an anharmonicity analysis in which the volume contribution to the total frequency shifts observed with temperature has been found very large for the internal modes. An abrupt change of slope in the frequency-versus-pressure diagrams of internal modes at 7 GPa is attributed to a stiffening of the LiF4-3 group. From the anharmonicity analysis, it is concluded that the internal binding in the LiF4-3 tetrahedra is essentially of ionic character. [S0163-1829(99)09805-7]. en
heal.publisher AMERICAN PHYSICAL SOC en
heal.journalName Physical Review B - Condensed Matter and Materials Physics en
dc.identifier.doi 10.1103/PhysRevB.59.4154 en
dc.identifier.isi ISI:000078699400031 en
dc.identifier.volume 59 en
dc.identifier.issue 6 en
dc.identifier.spage 4154 en
dc.identifier.epage 4162 en


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