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 |
|