Revealing the complex nature of bonding in binary high-pressure compound FeO
arXiv:1905.05497 · doi:10.1103/PhysRevLett.126.106001
Abstract
Extreme pressures and temperatures are known to drastically affect the chemistry of iron oxides resulting in numerous compounds forming homologous series FeOFeO and the appearance of FeO. Here, based on the results of \emph{in situ} single-crystal X-ray diffraction, Mössbauer spectroscopy, X-ray absorption spectroscopy, and DFT+dynamical mean-field theory calculations we demonstrate that iron in high pressure cubic FeO and isostructural FeOH is ferric (Fe), and oxygen has a formal valence less than two. Reduction of oxygen valence from 2, common for oxides, down to 1.5 can be explained by a formation of a localized hole at oxygen sites.
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- Valence Transition Theory of the Pressure-Induced Dimensionality Crossover in Superconducting SrCaCuO
- Interplay of electronic correlations and chemical bonding in FeN under pressure