Orbital structure and magnetic ordering in stoichiometric and doped crednerite CuMnO2

A. V. Ushakov, S. V. Streltsov, and D. I. Khomskii
Phys. Rev. B 89, 024406 – Published 10 January 2014

Abstract

The exchange interactions and magnetic structure in layered system CuMnO2 (mineral crednerite) and in nonstoichiometric system Cu1.04Mn0.96O2, with triangular layers distorted due to orbital ordering of the Mn3+ ions, are studied by ab initio band-structure calculations, which were performed within the GGA + U approximation. The exchange interaction parameters for the Heisenberg model within the Mn planes and between the Mn planes are estimated. We explain the observed in-plane magnetic structure by the dominant mechanism of the direct dd exchange between neighboring Mn ions. The superexchange via O ions, with 90 Mn–O–Mn bonds, plays a less important role for the in-plane exchange. The interlayer coupling is largely dominated by one exchange path between the half-filled 3z2r2 orbitals of Mn3+. The change of interlayer coupling from antiferromagnetic in pure CuMnO2 to ferromagnetic in doped material is also explained by our calculations.

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  • Received 3 October 2013
  • Revised 23 December 2013

DOI:https://doi.org/10.1103/PhysRevB.89.024406

©2014 American Physical Society

Authors & Affiliations

A. V. Ushakov1, S. V. Streltsov1,2, and D. I. Khomskii3

  • 1Institute of Metal Physics, Russian Academy of Science, S. Kovalevskaya Str. 18, 620041 Ekaterinburg, Russia
  • 2Ural Federal University, Mira St. 19, 620002 Ekaterinburg, Russia
  • 3II. Physikalisches Institut, Universität zu Köln, Zülpicher straße 77, D-50937 Köln, Germany

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Vol. 89, Iss. 2 — 1 January 2014

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