Coexisting magnetic structures and spin reorientation in Er0.5Dy0.5FeO3: Bulk magnetization, neutron scattering, specific heat, and density functional theory studies

Sarita Rajput, Padmanabhan Balasubramanian, Ankita Singh, Françoise Damay, C. M. N. Kumar, W. Tabis, T. Maitra, and V. K. Malik
Phys. Rev. B 105, 214436 – Published 28 June 2022

Abstract

The complex magnetic structures, spin reorientation, and associated exchange interactions have been investigated in Er0.5Dy0.5FeO3 using bulk magnetization, neutron diffraction, specific heat measurements, and density functional theory calculations. The Fe3+ spins order as G-type antiferromagnet structure depicted by Γ4(GxAyFz) irreducible representation below 700 K, similar to its end compounds. The bulk magnetization data indicate occurrence of the spin-reorientation and rare-earth magnetic moments' polarization below 75 K and 10 K, respectively. The neutron diffraction studies confirm an “incomplete” Γ4 Γ2(FxCyGz) spin-reorientation initiated 75 K. Although the relative volume fraction of the two magnetic structures varies with decreasing temperature, both coexist even at 1.5 K. Below 10 K, the polarization of Er3+/Dy3+ moments in a cyR arrangement develops, which gradually increases with decreasing temperature. At 2 K, magnetic structure associated with czR arrangement of Er3+/Dy3+ moments also appears. At 1.5 K, while the rare-earth magnetic moments show a cyR+czR-type arrangement, the Fe3+ spins are represented by a combination of a Γ2+Γ4 (Gz,Gx) arrangement. A clear signature of the magnetic structure with Γ1(Gy) representation, symmetrically compatible with the czR-type arrangement of rare-earth moments, is not confirmed from the refinement of the neutron diffraction data. The observed Schottky anomaly at 2.5 K suggests that the “rare-earth ordering” is induced by polarization due to Fe3+ spins. The Er3+Fe3+ and Er3+Dy3+ exchange interactions, obtained from first principle calculations, indicate that these interactions primarily cause the complicated spin reorientation and cyR rare-earth ordering in the system, respectively, while the dipolar interactions between rare-earth moments result in the czR type rare-earth ordering at 2 K.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
4 More
  • Received 3 October 2021
  • Revised 12 April 2022
  • Accepted 1 June 2022

DOI:https://doi.org/10.1103/PhysRevB.105.214436

©2022 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Sarita Rajput1, Padmanabhan Balasubramanian2, Ankita Singh1, Françoise Damay3, C. M. N. Kumar4,5, W. Tabis5, T. Maitra1, and V. K. Malik1,*

  • 1Department of Physics, Indian Institute of Technology Roorkee, Roorkee 247 667, India
  • 2Department of Physics, Graphic Era University, Dehradun, Uttarakhand 248 002, India
  • 3Laboratoire Léon Brillouin, CEA-CNRS, CEA/Saclay, 91191 Gif-sur-Yvette, France
  • 4Institute of Solid State Physics, Vienna University of Technology, Wiedner Hauptstrasse 8-10, 1040 Vienna, Austria
  • 5AGH University of Science and Technology, Faculty of Physics and Applied Computer Science, 30-059 Kraków, Poland

  • *vivek.malik@ph.iitr.ac.in

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 105, Iss. 21 — 1 June 2022

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review B

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×