Abstract
Using real-time spectroscopic ellipsometry, we directly observed a reversible lattice and electronic structure evolution in () epitaxial thin films. Drastically different electronic ground states, which are extremely susceptible to the oxygen content , are found in the two topotactic phases: i.e., the brownmillerite and the perovskite . First-principles calculations confirmed substantial differences in the electronic structure, including a metal-insulator transition, which originate from the modification in the Co valence states and crystallographic structures. More interestingly, the two phases can be reversibly controlled by changing the ambient pressure at greatly reduced temperatures. Our finding provides an important pathway to understanding the novel oxygen-content-dependent phase transition uniquely found in multivalent transition metal oxides.
- Received 13 February 2013
DOI:https://doi.org/10.1103/PhysRevLett.111.097401
© 2013 American Physical Society