2014
DOI: 10.1103/physrevb.90.195126
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Electronic structure and polaronic charge distributions of Fe vacancy clusters inFe1xO

Abstract: We perform a detailed study of the electronic structure of Fe 1−x O at moderate values of x. Our results evidence that the Fe vacancies introduce significant local modifications of the structural, electronic, and magnetic features, which serve to explain the origin of the measured dependencies of the physical properties on x. The final properties are determined by a complex interplay of the charge demand from O, the magnetic interactions, and the charge order at the Fe sublattice. Furthermore, polaronic distri… Show more

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Cited by 6 publications
(11 citation statements)
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References 54 publications
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“…This result corresponds very well to the recent findings presented in Ref. [15]. In principle, the divalent and trivalent Fe cations residing in the R and I sites of the wüstite lattice are distinguishable by methods sensitive to changes in the electronic structure of valence shell (e.g.…”
Section: Electronic Structuresupporting
confidence: 92%
See 1 more Smart Citation
“…This result corresponds very well to the recent findings presented in Ref. [15]. In principle, the divalent and trivalent Fe cations residing in the R and I sites of the wüstite lattice are distinguishable by methods sensitive to changes in the electronic structure of valence shell (e.g.…”
Section: Electronic Structuresupporting
confidence: 92%
“…Recently, it was shown that polaronic distributions of charge resembling those in magnetite Fe 3 O 4 emerge for the most stable defect structures in wüstite [15].…”
Section: Introductionmentioning
confidence: 99%
“…The Fe A model departs from the natural evolution of the rock- salt FeO(111) stacking to a spinel Fe 3 O 4 (111) structure, shifting one Fe cation from the outermost Fe layer to a tetrahedral coordination site (Fe A ) above the surface O plane. It also represents locally the surface environment corresponding to a 4:1 cluster of Fe vacancies 10 . As evidenced in the figure, the position of this Fe A cation relaxes to become almost coplanar to O, and the 1:1 Fe:O ratio is preserved at B1.…”
Section: Methodsmentioning
confidence: 99%
“…Previous studies of the FeO(111) surface have led a considerable dispersion of results, partly due to the difficulties to prepare high quality samples. On one hand, the bulk form only exists at ambient conditions with a significant 5-15% of Fe vacancies, and these vacancies tend to organize in different arrangements of local spinel-like clusters 10 . Though Fe 1−x O samples can be stabilized by fast quenching, it is difficult to discern these clusters from Fe 3 O 4 inclusions, which complicates their characterization.…”
Section: Introductionmentioning
confidence: 99%
“…6c), four Fe oct 2+ cations are replaced by one Fe tet 3+ interstitial. 41 Using this terminology, the SCV reconstruction can be viewed as an ordered array of subsurface 2 : 1 defect clusters. The cation-deficient structure at the Fe 3 O 4 (001) surface has particularly important consequences for the adsorption of 3d transition metals.…”
Section: Materials With Cation Vacancies: Iron Oxidesmentioning
confidence: 99%