Article Inverse exchange bias effects and magnetoelectric coupling of the half-doped perovskite-type chromites Gd0.5Sr0.5CrO3 and Gd0.5Ca0.5CrO3

Biswajit Dalal (National Institute for Materials Science) ; Xun Kang ORCID (National Institute for Materials Science) ; Yoshitaka Matsushita SAMURAI ORCID (National Institute for Materials Science) ; Alexei A. Belik SAMURAI ORCID (National Institute for Materials Science) ; Yoshihiro Tsujimoto SAMURAI ORCID (National Institute for Materials Science) ; Kazunari Yamaura SAMURAI ORCID (National Institute for Materials Science)

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Biswajit Dalal, Xun Kang, Yoshitaka Matsushita, Alexei A. Belik, Yoshihiro Tsujimoto, Kazunari Yamaura. Inverse exchange bias effects and magnetoelectric coupling of the half-doped perovskite-type chromites Gd0.5Sr0.5CrO3 and Gd0.5Ca0.5CrO3. Physical Review B. 2022, 106 (10), 104425. https://doi.org/10.48505/nims.4733
SAMURAI

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(abstract)

The Cr4+ oxidation state with two electrons in the Cr 3d 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 novel half-doped perovskite-type chromites Gd0.5Sr0.5CrO3 (GSCO) and Gd0.5Ca0.5CrO3 (GCCO). Fifty percent of the Cr occurs in the Cr4+ oxidation state following 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 (Pbnm) structures with different degrees of local lattice distortion. GSCO exhibits a long-range magnetic order at temperatures of <98 K, accompanied by magnetization reversal, suggesting that the magnetic ground state is ferrimagnetic. In contrast, GCCO displays antiferromagnetic characters at temperatures below approximately 100 K. In addition, GSCO exhibits a crossover between conventional and inverse exchange bias effects at low temperatures (<50 K). 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.

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Keyword: perovskite oxide, chromium, exchange bias effect

Date published: 2022-09-21

Publisher: American Physical Society (APS)

Journal:

  • Physical Review B (ISSN: 1550235X) vol. 106 issue. 10 104425

Funding:

  • Japan Society for the Promotion of Science JP20H05276
  • Japan Society for the Promotion of Science JP22H04601
  • Japan Synchrotron Radiation Research Institute 2020A4501
  • Japan Synchrotron Radiation Research Institute 2021A1169

Manuscript type: Author's version (Accepted manuscript)

MDR DOI: https://doi.org/10.48505/nims.4733

First published URL: https://doi.org/10.1103/physrevb.106.104425

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Updated at: 2024-09-10 12:30:18 +0900

Published on MDR: 2024-09-10 12:30:18 +0900

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