MOSSBAUER INVESTIGATIONS AND MOLECULAR ORBITAL CALCULATIONS ON EPIDOTE

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dc.contributor.author Grodzicki M.
dc.contributor.author Heuss-Assbichler S.
dc.contributor.author Amthauer G.
dc.date.accessioned 2021-03-15T05:26:56Z
dc.date.available 2021-03-15T05:26:56Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=812769
dc.identifier.citation Physics and Chemistry of Minerals, 2001, 28, 9, 675-681
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26713
dc.description.abstract The electronic structure of iron-rich epidote has been investigated by cluster molecular orbital calculations in local spin density approximation. Calculated quadrupole splittings for Fe(III) at both the M1 and M3 sites are in quantitative agreement with the experimental values obtained by Mossbauer spectroscopy. A detailed analysis of the theoretical results shows that a strong tetragonal compression of the M3 octahedron is responsible for the unusually large value of the quadrupole splitting of FeM3I). The corresponding electric field gradient (efg) is dominated by the anisotropy of the valence shell of iron, whereas the ligands contribute only about 15% to the efg. The calculations emphasize that rather large clusters, extending beyond the second coordination sphere of iron, are necessary for a reliable description. Small clusters including only the first coordination sphere of iron generally yield misleading results due to unsaturated oxygen bonds and relatively large cluster charges.
dc.subject EPIDOTE
dc.subject MOLECULAR ORBITAL CALCULATIONS
dc.subject MOSSBAUER SPECTROSCOPY
dc.title MOSSBAUER INVESTIGATIONS AND MOLECULAR ORBITAL CALCULATIONS ON EPIDOTE
dc.type Статья


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