Abstract
We present the magnetic structure of , solved via neutron powder diffraction. We demonstrate that long-range magnetic order develops below 74 K, and at 28 K a spin-flop transition occurs driven by exchange and rare-earth single-ion anisotropy. In both magnetic phases, the magnetic structure may be described as a collinear ferrimagnet, contrary to conventional theories of magnetic order in the manganite perovskites. Instead, we show that these magnetic structures can be understood to arise due to ferro-orbital order, the , and site point symmetry, , and the dominance of exchange over both and exchange, which together are unique to the perovskites.
- Received 18 January 2019
- Revised 1 March 2019
DOI:https://doi.org/10.1103/PhysRevB.99.104424
©2019 American Physical Society