Theoretical and experimental evidence of a site-selective Mott transition in Fe2O3 under pressure
arXiv:1706.02787 · doi:10.1103/PhysRevX.8.031059
Abstract
We provide experimental and theoretical evidence for a novel type of pressure-induced insulator-metal transition characterized by site-selective delocalization of the electrons. Mössbauer spectroscopy, X-ray diffraction and electrical transport measurements on FeO to 100 GPa, along with dynamical mean-field theory (DFT+DMFT) calculations, reveal this site-selective Mott transition between 50 and 68 GPa, such that the metallization can be described by ($^\rm{VI}$Fe)O [ structure] ($^\rm{VIII}$FeFe$^\rm{M}$)O [ structure] ($^\rm{VI}$Fe$^\rm{M}$)O [ structure]. Within the crystal structure, characterized by two distinct coordination sites (VI and VIII), we observe equal abundances of ferric ions (Fe) and ions having delocalized electrons (Fe$^\rm{M}$), and only at higher pressures is a fully metallic structure obtained, all at room temperature. The transition is characterized by delocalization/metallization of the electrons on half the Fe sites, with a site-dependent collapse of local moments. Above 50 GPa, FeO is a strongly correlated metal with reduced electron mobility (large band renormalizations) of m*/m4 and 6 near the Fermi level. Upon decompression, we observe a site-selective (metallic) to conventional Mott insulator phase transition ($^\rm{VIII}$FeFe$^\rm{M}$)O ($^\rm{VIII}$FeFe)O within the same structure, indicating a decoupling of the electronic and lattice degrees of freedom, characteristic of a true Mott transition. Our results show that the interplay of electronic correlations and lattice may result in rather complex behavior of the electronic structure and magnetic state.
18 pages, 5 figures
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