Abstract
The minerals versiliaite and apuanite have been synthesised for the first time. The 57Fe Mössbauer spectra recorded at 298 and 4 K are reported. The results are indicative of a formulation for versiliaite as \(\left (\text {Fe}_{4}^{2+}\text {Fe}_{4}^{3+}\right )^{\text {oct}}\left [\text {Fe}_{4}^{3+}\text {Sb}_{12}^{3+}\right ]^{\text {tet}}\textit {O}_{32}\textit {S}_{2}\) and of apuanite as \(\left (\text {Fe}_{4}^{2+}\text {Fe}_{8}^{3+}\right )^{\text {oct}}\left [\text {Fe}_{8}^{3+}\text {Sb}_{16}^{3+}\right ]^{\text {tet}}\textit {O}_{48}\textit {S}_{\mathrm {4.}}\) The spectra recorded at low temperature are indicative of complex magnetic interactions. The results indicate the potential for the synthesis of further new structurally-related materials with different compositions and new low dimensional physical properties.
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This article is part of the Topical Collection on Proceedings of the 2nd Mediterranean Conference on the Applications of the Mössbauer Effect (MECAME 2016), Cavtat, Croatia, 31 May-3 June 2016
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Bayliss, R.D., Berry, F.J., Cumby, J.C. et al. Synthetic versiliaite and apuanite: investigation by 57Fe Mössbauer spectroscopy. Hyperfine Interact 237, 98 (2016). https://doi.org/10.1007/s10751-016-1308-3
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DOI: https://doi.org/10.1007/s10751-016-1308-3