Abstract
The oxidation state with two electrons in the shell is not often observed in perovskite-type oxides, as high pressures and temperatures are generally required to stabilize the octahedral coordination. Herein, we present a comparative study of the half-doped perovskite-type chromites (GSCO) and (GCCO). Fifty percent of the Cr occurs in the oxidation state after high-pressure synthesis at 6 GPa and 1200 °C. The materials were investigated using synchrotron x-ray diffraction, magnetization, heat capacity, and dielectric measurements. The diffraction patterns show that GSCO and GCCO crystallize in orthorhombic () structures with different degrees of local lattice distortion. GSCO exhibits a long-range magnetic order at temperatures of , accompanied by magnetization reversal, suggesting that the magnetic ground state is ferrimagnetic. In contrast, GCCO displays antiferromagnetic characters at temperatures . In addition, GSCO exhibits a crossover between conventional and inverse exchange bias effects at low temperatures (). This is likely caused by asymmetric exchange Dzyaloshinskii-Moriya interactions between the Cr ions of different valences (+3 and +4). Furthermore, significant magnetoelectric coupling at the onset of the magnetic order is supported by temperature-dependent dielectric measurements.
6 More- Received 28 May 2022
- Revised 31 July 2022
- Accepted 9 September 2022
DOI:https://doi.org/10.1103/PhysRevB.106.104425
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