MOSSBAUER INVESTIGATIONS AND MOLECULAR ORBITAL CALCULATIONS ON EPIDOTE

dc.contributor.authorGrodzicki M.
dc.contributor.authorHeuss-Assbichler S.
dc.contributor.authorAmthauer G.
dc.date.accessioned2021-03-15T05:26:56Z
dc.date.available2021-03-15T05:26:56Z
dc.date.issued2001
dc.description.abstractThe 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.identifierhttps://www.elibrary.ru/item.asp?id=812769
dc.identifier.citationPhysics and Chemistry of Minerals, 2001, 28, 9, 675-681
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26713
dc.subjectEPIDOTE
dc.subjectMOLECULAR ORBITAL CALCULATIONS
dc.subjectMOSSBAUER SPECTROSCOPY
dc.titleMOSSBAUER INVESTIGATIONS AND MOLECULAR ORBITAL CALCULATIONS ON EPIDOTE
dc.typeСтатья

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