Abstract
Synchrotron x-ray-diffraction patterns were measured and analyzed for a polycrystalline sample of the room-temperature ferromagnet from , from which two structural phase transitions were found to occur successively. The higher-temperature transition at is driven by ordering of the oxygen vacancies, which is closely related to the metallic state at high temperatures. The lower-temperature transition at is of first order, at which the ferromagnetic state suddenly appears exhibiting a jump in magnetization and resistivity. Based on the refined structure, possible spin and orbital models for the magnetic order are proposed.
- Received 17 May 2007
DOI:https://doi.org/10.1103/PhysRevB.75.220406
©2007 American Physical Society