Twofold spin reorientation and field-induced incomplete phase transition in single-crystal Dy0.5Pr0.5FeO3

Hailong Wu, Shixun Cao, Ming Liu, Yiming Cao, Baojuan Kang, Jincang Zhang, and Wei Ren
Phys. Rev. B 90, 144415 – Published 13 October 2014

Abstract

We report an intriguing twofold spin reorientation transition of type Γ4(Gx,Ay,Fz)Γ1(Ax,Gy,Cz)Γ2(Fx,Cy,Gz) for the Fe3+ magnetic sublattice near spin reorientation temperatures TSR177 K and TSR245 K in a rare-earth orthoferrite Dy0.5Pr0.5FeO3 single crystal. Magnetic-field-induced incomplete spin-configuration transitions (Γ4Γ41Γ42 for H =20kOe and Γ4Γ42 for H =40kOe) were observed by measurement of magnetization as a function of temperature. The spin reorientation temperature of a Dy0.5Pr0.5FeO3 single crystal can be controlled by changing the magnitude of the applied magnetic field. We also show that spin reorientation of the Γ1Γ4 type between TSR2 and TSR1 can be induced by an applied magnetic field along the c axis. The origin of the intriguing magnetic behavior is ascribed to the anisotropic effective field whose strength is determined by the interactions with R3+(R =Dy,Pr) spins and can be modified by the external applied magnetic field. It provides deeper insight into the Fe3+R3+ magnetic interaction which dominates the sophisticated magnetic phase transitions in the rare-earth orthoferrites.

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  • Received 9 June 2014
  • Revised 18 September 2014

DOI:https://doi.org/10.1103/PhysRevB.90.144415

©2014 American Physical Society

Authors & Affiliations

Hailong Wu, Shixun Cao*, Ming Liu, Yiming Cao, Baojuan Kang, Jincang Zhang, and Wei Ren

  • Department of Physics, and International Center of Quantum and Molecular Structures, Shanghai University, Shanghai 200444, China

  • *Corresponding author: sxcao@shu.edu.cn
  • renwei@shu.edu.cn

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Vol. 90, Iss. 14 — 1 October 2014

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