Abstract
Variations of perovskite superstructure type and magnetic properties across the high-pressure series have been investigated by powder neutron-diffraction, x-ray magnetic circular dichroism, and magnetization measurements. Monoclinic double perovskite solid solutions with rocksalt-type ordering of cations but no -cation order are discovered to exist only close to the end members and . Compositions in the range adopt a tetragonal double-double perovskite phase based on , which has both columnar and rocksalt cation orders. Two-phase coexistence of double and double-double perovskites occurs over wide regions between these limits. All samples are ferrimagnetic with Curie temperatures near 500 K. Low-temperature Mn spin order is also observed in the Mn-rich double perovskites and the double-double perovskites. Spin reorientation transitions observed across all of the double perovskites are shown to result from orbital ordering, but this does not occur in the double-double perovskites. The Ca-rich double perovskites show significant magnetic coercivity at low temperatures.
1 More- Received 7 April 2020
- Revised 11 May 2020
- Accepted 15 May 2020
DOI:https://doi.org/10.1103/PhysRevMaterials.4.064408
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