Abstract
First-principles density functional calculations on the metal-insulator transition (MIT) in perovskite CaFeO point to local ferromagnetic coupling as the microscopic origin for the electronic “charge order” transition. Our atomic, electronic, and magnetic structure analyses reveal that the MIT results from a spin-assisted covalent bonding mechanism between the O 2 and Fe 3 states with anisotropic Fe-O bonds and negligible intersite Fe-Fe charge transfer. We suggest that control of the lattice distortions, which mediate the covalent bond formation, in oxides containing late transition-metal row cations in high valence states provides a platform to tailor electronic transitions.
- Received 20 June 2012
DOI:https://doi.org/10.1103/PhysRevB.86.195144
©2012 American Physical Society