Abstract
This work reports on the evaluation of the electric field gradient (EFG) in natural chrysoberyl Al2BeO4 and sinhalite MgAlBO4 using two different procedures: (1) experimental, with single crystal Mössbauer spectroscopy (SCMBS) on the three principal sections of each sample and (2) a “fully quantitative” method with cluster molecular orbital calculations based on the density functional theory. Whereas the experimental and theoretical results for the EFG tensor are in quantitative agreement, the calculated isomer shifts and optical d–d-transitions exhibit systematic deviations from the measured values. These deviations indicate that the substitution of Al and Mg with iron should be accompanied by considerable local expansion of the coordination octahedra.
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Acknowledgments
The authors thank W. Waldhör, Salzburg, for providing the polishing of the natural chrysoberyl and sinhalite single crystal cuts. All calculations were carried out at the Department of Computer Sciences in Salzburg. Financial support by the Austrian Fund for Scientific Research (FWF) under the grant number P18329-N20 is gratefully acknowledged.
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Lottermoser, W., Redhammer, G.J., Weber, SU. et al. The electric field gradient in natural iron-doped chrysoberyl Al2BeO4 and sinhalite MgAlBO4 single crystals. Phys Chem Minerals 38, 787–799 (2011). https://doi.org/10.1007/s00269-011-0451-2
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DOI: https://doi.org/10.1007/s00269-011-0451-2