Abstract
The Mössbauer spectra of a nearly stoichiometric natural bornite, Cu5FeS4, specimen were reinvestigated between 295 and 4.2 K. There is no difference between the Neél temperature T N as determined by the Mössbauer effect or by the susceptibility measurements (T N = 67.5 K). No additional paramagnetic doublet can be observed in the low-temperature MS spectra. The valence state of Fe is Fe(3−x)+ caused by a partial electron transfer from the Cu+ ions to the Fe3+ ions which increases the shielding of the s-electrons by the d-electron density and by this increases the isomer shift to a value intermediate between tetrahedral high-spin Fe2+ and tetrahedral high-spin Fe3+.
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Authors acknowledge the Departments of Chemistry and of Earth Sciences of the University of Florence, for funding this research under the ex-60% programme, and the Italian CNR, for support.
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Borgheresi, M., Di Benedetto, F., Romanelli, M. et al. Mössbauer study of bornite and chemical bonding in Fe-bearing sulphides. Phys Chem Minerals 45, 227–235 (2018). https://doi.org/10.1007/s00269-017-0911-4
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DOI: https://doi.org/10.1007/s00269-017-0911-4