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SrV0.3Fe0.7O2.8: A Vacancy-Ordered Fe-Based Perovskite Exhibiting Room-Temperature Magnetoresistance.
Nagase, Teppei; Nishikubo, Takumi; Fukuda, Masayuki; Sakai, Yuki; Shigematsu, Kei; Ikeda, Yoichi; Nambu, Yusuke; Zhang, Qiang; Matsuda, Masaaki; Mibu, Ko; Azuma, Masaki; Yamamoto, Takafumi.
Afiliação
  • Nagase T; Laboratory for Materials and Structures, Tokyo Institute of Technology, Midori-ku, Yokohama 226-8503, Japan.
  • Nishikubo T; Laboratory for Materials and Structures, Tokyo Institute of Technology, Midori-ku, Yokohama 226-8503, Japan.
  • Fukuda M; Kanagawa Institute of Industrial Science and Technology, Ebina 243-0435, Japan.
  • Sakai Y; Laboratory for Materials and Structures, Tokyo Institute of Technology, Midori-ku, Yokohama 226-8503, Japan.
  • Shigematsu K; Laboratory for Materials and Structures, Tokyo Institute of Technology, Midori-ku, Yokohama 226-8503, Japan.
  • Ikeda Y; Kanagawa Institute of Industrial Science and Technology, Ebina 243-0435, Japan.
  • Nambu Y; Laboratory for Materials and Structures, Tokyo Institute of Technology, Midori-ku, Yokohama 226-8503, Japan.
  • Zhang Q; Kanagawa Institute of Industrial Science and Technology, Ebina 243-0435, Japan.
  • Matsuda M; Institute for Materials Research, Tohoku University, Sendai 980-8577, Japan.
  • Mibu K; Institute for Materials Research, Tohoku University, Sendai 980-8577, Japan.
  • Azuma M; Organization for Advanced Studies, Tohoku University, Sendai 980-8577, Japan.
  • Yamamoto T; FOREST, Japan Science and Technology Agency, Kawaguchi, Saitama 332-0012, Japan.
Inorg Chem ; 2022 Jun 03.
Article em En | MEDLINE | ID: mdl-35657337
ABSTRACT
We report room-temperature (RT) magnetoresistance (MR) in a novel Fe-based perovskite, SrV0.3Fe0.7O2.8. This compound contains ordered oxygen vacancies in every fifth primitive perovskite (111)p plane, leading to a layered structure consisting of triple-octahedral and double-tetrahedral layers. Along with the oxygen vacancies, the transition-metal ions are also ordered the octahedral sites are occupied by 100% of Fe ions, while the tetrahedral sites are occupied by 25% of Fe ions and 75% of V ions. As a result, SrV0.3Fe0.7O2.8 forms a magnetically striped lattice in which the octahedral layers with 100% of magnetic Fe ions are separated by the diluted magnetic layer. The compound exhibits weak ferromagnetism and shows a large negative MR (-5% at 3 T) at RT, despite the small saturation moment (0.4 µB/Fe atom). Thus, this type of layered compound is promising for further large MR by an increase of magnetization through chemical substitution.

Texto completo: 1 Base de dados: MEDLINE Idioma: En Revista: Inorg Chem Ano de publicação: 2022 Tipo de documento: Article País de afiliação: Japão

Texto completo: 1 Base de dados: MEDLINE Idioma: En Revista: Inorg Chem Ano de publicação: 2022 Tipo de documento: Article País de afiliação: Japão