Pressure-induced ferromagnetism in cubic perovskite SrFeO3 and BaFeO3

Zhi Li, Toshiaki Iitaka, and Takami Tohyama
Phys. Rev. B 86, 094422 – Published 17 September 2012

Abstract

The spin order in cubic perovskite SrFeO3 and BaFeO3 under high pressure is studied by density functional theory (DFT) calculation with local spin density approximation plus Hubbard U (LSDA+U). At ambient pressure, A-type and G-type helical spin orders are almost degenerate in BaFeO3 whose lattice constant is 3.97 Å. When the lattice constant is reduced to 3.85 Å, which is the same as the lattice constant of SrFeO3 at ambient pressure, G-type helical spin order becomes stable, being consistent with SrFeO3. This is because superexchange interaction is enhanced as compared with double-exchange interaction. Phase transition from helical spin state to ferromagnetic state in both SrFeO3 and BaFeO3 takes place if the lattice constant is further reduced to 3.70 Å. This is because reduced local spin moment weakens the contribution from superexchange interaction. Our result agrees with recent experimental result of BaFeO3 under high pressure. Additionally, our calculation predicts that half-metal BaFeO3 at ambient pressure will become a good metal under high pressure.

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  • Received 21 May 2012

DOI:https://doi.org/10.1103/PhysRevB.86.094422

©2012 American Physical Society

Authors & Affiliations

Zhi Li1, Toshiaki Iitaka2, and Takami Tohyama1

  • 1Yukawa Institute for Theoretical Physics, Kyoto University, Kyoto 606-8502, Japan
  • 2Computational Astrophysics Laboratory, RIKEN, 2-1 Hirosawa, Wako, Saitama 351-0198, Japan

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Vol. 86, Iss. 9 — 1 September 2012

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