Abstract
Transport and magnetic properties of polycrystalline have revealed the existence of two distinguishable monoclinic ferromagnetic phases separated by a two-phase domain and a pseudotetragonal phase with that was prepared at 600 °C. A nearly oxygen-stoichiometric sample having a magnetization with a Curie temperature is identified as atomically ordered containing about 1.8% antiferromagnetic spins at antisites. This ferromagnetic phase is an n-type polaronic conductor that progressively traps mobile electrons at the oxygen vacancies that introduced them on lowering the temperature. Although the x-ray-diffraction pattern can be indexed in orthorhombic (Pbnm) or monoclinic symmetry with atomic order identifies the space group as A second monoclinic, ferromagnetic phase with and has a large, positive thermoelectric power that increases progressively with decreasing temperature. Quenching a sample from 1350 °C into liquid gave a single phase with and A sample with that was synthesized at 600 °C was pseudotetragonal and had a paramagnetic Weiss constant as well as a significantly smaller magnetization, but its magnetization curve showed no evidence of spin-glass behavior; its large, positive thermoelectric power was characteristic of polaronic conduction without trapping of mobile charge carriers at lower temperatures. Interpretation of the two phases with is based on the hypothesis that introduction of high-spin by the oxygen vacancies creates around it additional and intermediate-spin at neighboring sites; the resulting gain in elastic energy from cooperative, dynamic Jahn-Teller deformations at these ions must be sufficient to overcome the cost of about 0.2 eV for the electron transfer from a to a
- Received 16 May 2002
DOI:https://doi.org/10.1103/PhysRevB.67.014401
©2003 American Physical Society