paper

Phase diagram description of the CaCuFeO double perovskite

arXiv:1804.05726 · doi:10.1063/1.5032206

Abstract

CaCuFeO exhibits a temperature-induced transition from a ferrimagnetic-insulating phase, in which Fe appears charge disproportionated, as Fe and Fe, to a paramagnetic-metallic phase at temperatures above 210 K, with Fe present. To describe it, we propose a microscopic effective model with two interpenetrating sublattices of Fe and Fe, respectively, being the Fe-charge disproportionation. We include all -Fe orbitals: localized orbitals, with spin 3/2 and magnetically coupled, plus two degenerate itinerant orbitals with local and nearest-neighbor (NN) electron correlations, and hopping between NN orbitals of the same symmetry. Allub and Alascio previously proposed a model to describe the phase transition in LaCuFeO from a paramagnetic-metal to an antiferromagnetic-insulator, induced by temperature or pressure, involving charge transfer between Fe and Cu ions, in contrast to Fe-charge disproportionation. With the model proposed for CaCuFeO, modified to account for this difference between the two compounds, the density of states of the itinerant Fe orbitals was obtained, using Green's functions methods. The phase diagram for CaCuFeO was calculated, including phases exhibiting Fe-charge disproportionation, where the two eg orbitals in each site are symmetrically occupied, as well as novel phases exhibiting local orbital selectivity/asymmetric occupation of orbitals. Both kinds of phases may exhibit paramagnetism and ferromagnetism. We determined the model parameters which best describe the phase transition observed in CaCuFeO, and found other phases at different parameter ranges, which might be relevant for other compounds of the ACuFeO family, which present both types of transitions.

11 pages, 12 figures