Fe2+-O and Mn2+-O bonding and Fe2+- and Mn2+-vibrational properties in synthetic almandine-spessartine solid solutions: an X-ray absorption rine structure study.

Sani, A., Quartieri, S., Boscherini, F., Antonioli, G., Feenstra, A. and Geiger, C. A. (2004) Fe2+-O and Mn2+-O bonding and Fe2+- and Mn2+-vibrational properties in synthetic almandine-spessartine solid solutions: an X-ray absorption rine structure study. European Journal of Mineralogy, 16 (5). pp. 801-808. DOI 10.1127/0935-1221/2004/0016-0801.

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Abstract

X-ray absorption fine structure (XAFS) measurements at the Fe and Mn K-edges were undertaken to investigate the Fe2+-O and Mn2+-O bonding, and Fe2+- and Mn2+-vibrational properties for a series of synthetic almandine-spessartine, (Fe,Mn)(3)Al2Si3O12, garnet solid solutions. The two end members almandine, Fe3Al2Si3O12, and spessartine, Mn3Al2Si3O12, and three solid solutions of composition Alm75Sps25, Alm50Sps50 and Alm25Sps75 were studied at different temperatures between 77 K and 423 K. The spectra show that the state of alternating bonds provides an appropriate description for the two crystallographic ally independent X-O(1) and X-O(2) bonds in the solid solution. An exchange of X-site cations in garnet is associated with measurable structural relaxation. The compositional and temperature dependence of the XAFS Debye-Waller factors for Fe2+ and Mn2+ in the plane of the X-O(1) and the X-O(2) bonds were also determined. Their values in the plane of the X-O(2) bonds are greater compared to those for X-O(1) and they do not vary greatly as a function of garnet composition. In the case of end-member spessartine, the XAFS Debye-Waller factors for Mn2+ are compared to the Debye-Waller factors measured from single-crystal X-ray diffraction. An analysis shows correlation in the atomic displacements along the shorter Mn-O(1) bond.

Document Type: Article
Keywords: garnet XAFS silicate solid solutions local-site distortion Debye-Waller factor multiple-scattering calculations al k-edge fine-structure xafs characterization grossular garnets crystal-chemistry mixing properties silicate garnets pyrope site
Research affiliation: Kiel University
Refereed: No
Date Deposited: 24 Jan 2012 05:41
Last Modified: 23 Sep 2019 18:57
URI: https://oceanrep.geomar.de/id/eprint/16165

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