Abstract
Structural and magnetic properties of the system have been systematically investigated. Initial samples were prepared via a sol-gel method. A pure hexagonal phase was only obtained for samples with . With high-pressure annealing, a pure orthorhombic perovskite phase was achieved for all the compositions. The Mössbauer spectrum for shows that only ions exist in the system; there was no evidence of chemical inhomogeneities. With increasing , the Néel temperature increases for both hexagonal and orthorhombic phases. The orthorhombic shows an interesting weak ferromagnetic state in the temperature range of , the ferromagnetism disappearing abruptly on cooling below . The transition at appears to be a reorientation of the spin axis of a type- antiferromagnetic order from the orthorhombic axis to the axis in the (010) plane.
- Received 12 March 2007
DOI:https://doi.org/10.1103/PhysRevB.76.174405
©2007 American Physical Society