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dc.contributor.author | Galeev A. | |
dc.contributor.author | Khasanova N. | |
dc.contributor.author | Rudowicz C. | |
dc.contributor.author | Shakurov G. | |
dc.contributor.author | Bulka G. | |
dc.contributor.author | Nizamutdinov N. | |
dc.contributor.author | Vinokurov V. | |
dc.date.accessioned | 2018-09-17T20:55:04Z | |
dc.date.available | 2018-09-17T20:55:04Z | |
dc.date.issued | 2004 | |
dc.identifier.issn | 0937-9347 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/134255 | |
dc.description.abstract | An electron paramagnetic resonance (EPR) study of a synthetic single crystal of LiScGeO4 doped with Cr ions carried out earlier at the X- and Q-bands at 300 K has indicated additional weak lines. A detailed analysis of these EPR lines, which were tentatively attributed to the Fe3+ ions at two different mirror symmetry sites, is presented in this paper. The angular dependences in the three crystallographic planes were resolved by fitting the two distinct spectra denoted Fe3+(I) and Fe3+(II) with a spin Hamiltonian (S = 5/2) of monoclinic symmetry. The rank-4 crystal field tensors at tetrahedral and octahedral sites were calculated with the point-charge model to determine the principal axis orientations of their cubic, tetragonal and trigonal components. A comparative analysis of the zero-field splitting tensors and the crystal field ones indicates that Fe3+(I) ions substitute for Sc3+ at octahedral sites and Fe3+(II) ions substitute for Ge4+ at tetrahedral sites with no significant distortion of the coordination polyhedra in the structure of LiScGeO 4. | |
dc.relation.ispartofseries | Applied Magnetic Resonance | |
dc.title | Electron paramagnetic resonance study of Fe3+ ions at octahedral and tetrahedral mirror symmetry sites in the LiScGeO4 crystal | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 4 | |
dc.relation.ispartofseries-volume | 26 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 533 | |
dc.source.id | SCOPUS09379347-2004-26-4-SID6444226775 |