Successive spin reorientations and rare earth ordering in Nd0.5Dy0.5FeO3: Experimental and ab initio investigations

Ankita Singh, Sarita Rajput, Padmanabhan Balasubramanian, M. Anas, Francoise Damay, C. M. N. Kumar, Gaku Eguchi, A. Jain, S. M. Yusuf, T. Maitra, and V. K. Malik
Phys. Rev. B 102, 144432 – Published 21 October 2020

Abstract

In the present paper, the magnetic structure and spin reorientation of mixed rare-earth orthoferrite Nd0.5Dy0.5FeO3 have been investigated. At room temperature, our neutron-diffraction measurements reveal that the magnetic structure of Fe3+ spins in Nd0.5Dy0.5FeO3 belongs to Γ4 irreducible representation (Gx, Fz) as observed in both parent compounds (NdFeO3 and DyFeO3). The neutron-diffraction study also confirms the presence of a spin-reorientation transition where the magnetic structure of Fe3+ spins changes from Γ4 to Γ2(Fx, Gz) representation between 75 and 20 K while maintaining a G-type antiferromagnetic configuration. Such a gradual spin reorientation is unusual since the large single ion anisotropy of Dy3+ ions is expected to cause an abrupt Γ4Γ1(Gy) rotation of the Fe3+ spins. At 10 K, the Fe3+ magnetic structure is represented by Γ2 (Fx, Gz). Unexpectedly, the Γ4 structure of Fe3+ spins re-emerges below 10 K, which also coincides with the development of rare-earth (Nd3+/Dy3+) magnetic ordering having cyR configuration. Such re-emergence of a magnetic structure has been a rare phenomenon in orthoferrites. The absence of a second-order phase transition in rare-earth ordering, interpreted from heat capacity data, suggests the prominent role of Nd3+Fe3+ and Nd3+Dy3+ exchange interactions. These interactions suppress the independent rare-earth magnetic ordering observed in both parent compounds due to Nd3+/Dy3+Nd3+/Dy3+ exchange interactions. Our density-functional-theory calculations including Coulomb correlation and spin-orbit interaction effects (DFT+U+SO) reveal that the C-type arrangement of rare-earth ions (Nd3+/Dy3+), with Γ2 (Fx, Gz) configuration for Fe3+ moments, is energetically very close to a phase with the same rare-earth magnetic ordering but Γ4 (Gx, Fz) configuration of Fe3+ spins. Further, the Nd3+Fe3+ and Nd3+Dy3+ exchange interactions are observed to play significant roles in the complex Fe3+ spin reorientation with the re-emergence of Γ4 at low temperature. Consistent with the experimental observations, our calculations established the mixed phase (Γ2 and Γ4) to be the magnetic ground state of Fe3+ moments.

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  • Received 29 June 2020
  • Revised 9 September 2020
  • Accepted 9 September 2020

DOI:https://doi.org/10.1103/PhysRevB.102.144432

©2020 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Ankita Singh1,*, Sarita Rajput1,*, Padmanabhan Balasubramanian2,*, M. Anas1, Francoise Damay3, C. M. N. Kumar4,5, Gaku Eguchi4, A. Jain6,7, S. M. Yusuf6,7, T. Maitra1, and V. K. Malik1,†

  • 1Department of Physics, Indian Institute of Technology Roorkee, Roorkee 247 667, India
  • 2Graphic Era University, Dehradun 248002, India
  • 3Laboratoire Léon Brillouin, CEA-CNRS, CEA/Saclay, 91191 Gif sur Yvette, France
  • 4Institute of Solid State Physics, Vienna University of Technology, Wiedner Hauptstr. 8-10/138, 1040 Vienna, Austria
  • 5AGH University of Science and Technology, Faculty of Physics and Applied Computer Science, 30-059 Kraków, Poland
  • 6Solid State Physics Division, Bhabha Atomic Research Center, Mumbai, 400 085, India
  • 7Homi Bhabha National Institute, Anushaktinagar, Mumbai 400 094, India

  • *These authors contributed equally to this work.
  • vivek.malik@ph.iitr.ac.in

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Vol. 102, Iss. 14 — 1 October 2020

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