We report results from high-pressure single-crystal X-ray diffraction and Mossbauer absorption experiments on magnetite. Based on high-quality diffraction data, we have obtained accurate information on the crystal structure of magnetite below 25 GPa, which enables an unambiguous interpretation of the Mossbauer data using constrained area ratios and a full transmission integral fit that avoids area distortion due to thickness effects. Based on our analysis, all aspects of the electronic and magnetic properties of magnetite reported previously below 25 GPa at ambient temperature can be explained solely by the enhanced delocalization of 3d electrons of iron atoms. For instance, we present evidence that the compression-induced metallization changes the sign of the charge carrier spin polarization at 15 GPa.

Effect of high pressure on the crystal structure and electronic properties of magnetite below 25 GPa / K. Glazyrin, C. McCammon, L. Dubrovinsky, M. Merlini, K. Schollenbruch, A. Woodland, M. Hanfland. - In: AMERICAN MINERALOGIST. - ISSN 0003-004X. - 97:1(2012), pp. 128-133. [10.2138/am.2011.3862]

Effect of high pressure on the crystal structure and electronic properties of magnetite below 25 GPa

M. Merlini;
2012

Abstract

We report results from high-pressure single-crystal X-ray diffraction and Mossbauer absorption experiments on magnetite. Based on high-quality diffraction data, we have obtained accurate information on the crystal structure of magnetite below 25 GPa, which enables an unambiguous interpretation of the Mossbauer data using constrained area ratios and a full transmission integral fit that avoids area distortion due to thickness effects. Based on our analysis, all aspects of the electronic and magnetic properties of magnetite reported previously below 25 GPa at ambient temperature can be explained solely by the enhanced delocalization of 3d electrons of iron atoms. For instance, we present evidence that the compression-induced metallization changes the sign of the charge carrier spin polarization at 15 GPa.
High pressure; Magnetite; Mössbauer spectroscopy; Single-crystal X-ray diffraction
Settore GEO/06 - Mineralogia
2012
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/222981
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