Structural transformation and magnetic competition in Yb(Mn1xFex)O3

Yun-Hui Huang, Maarit Karppinen, Naoki Imamura, Hisao Yamauchi, and John B. Goodenough
Phys. Rev. B 76, 174405 – Published 2 November 2007

Abstract

Structural and magnetic properties of the Yb(Mn1xFex)O3 (0x1) system have been systematically investigated. Initial samples were prepared via a sol-gel method. A pure hexagonal phase was only obtained for samples with x0.5. With high-pressure annealing, a pure orthorhombic perovskite phase was achieved for all the compositions. The Fe57 Mössbauer spectrum for x=0.5 shows that only Fe3+ ions exist in the system; there was no evidence of chemical inhomogeneities. With increasing x, the Néel temperature TN increases for both hexagonal and orthorhombic phases. The orthorhombic Yb(Mn0.5Fe0.5)O3 shows an interesting weak ferromagnetic state in the temperature range of 239298K, the ferromagnetism disappearing abruptly on cooling below Tt=239K. The transition at Tt appears to be a reorientation of the spin axis of a type-G antiferromagnetic order from the orthorhombic a axis to the b axis in the (010) plane.

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  • Received 12 March 2007

DOI:https://doi.org/10.1103/PhysRevB.76.174405

©2007 American Physical Society

Authors & Affiliations

Yun-Hui Huang1,2,*, Maarit Karppinen1,3, Naoki Imamura1, Hisao Yamauchi1, and John B. Goodenough2

  • 1Materials and Structures Laboratory, Tokyo Institute of Technology, Yokohama 226-8503, Japan
  • 2Texas Materials Institute, ETC 9.102, The University of Texas at Austin, Austin, Texas 78712, USA
  • 3Laboratory of Inorganic and Analytical Chemistry, Helsinki University of Technology, FI-02015 TKK, Finland

  • *yunhuihuang@yahoo.com

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Issue

Vol. 76, Iss. 17 — 1 November 2007

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