Magnetic coupling parameters at an oxide-oxide interface from first principles: Fe2O3-FeTiO3

Hasan Sadat Nabi, Richard J. Harrison, and Rossitza Pentcheva
Phys. Rev. B 81, 214432 – Published 21 June 2010

Abstract

Charge mismatch at the interface between canted antiferromagnetic hematite (α-Fe2O3) and antiferromagnetic ilmenite (FeTiO3) is accommodated by the formation of mixed Fe2+ and Fe3+ contact layers, leading to uncompensated magnetic moments in the system. To derive the magnetic exchange interaction parameters of the end members and interface, we map total-energy differences of collinear spin arrangements obtained from density-functional theory calculations to a Heisenberg Hamiltonian using the least-squares method. Parameters for the end members, hematite (Jm3+,3+) and ilmenite (Jm2+,2+) are in good agreement with the values obtained from inelastic neutron-scattering data. The magnetic interaction parameters between Fe2+ and Fe3+ (Jm2+,3+) in the contact layer show a strong antiferromagnetic coupling to the adjacent hematite layers and thus explain the ferrimagnetism in the system.

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  • Received 26 December 2009

DOI:https://doi.org/10.1103/PhysRevB.81.214432

©2010 American Physical Society

Authors & Affiliations

Hasan Sadat Nabi1,*, Richard J. Harrison2, and Rossitza Pentcheva1

  • 1Department of Earth and Environmental Sciences, Section Crystallography, University of Munich, Theresienstr. 41, 80333 Munich, Germany
  • 2Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, United Kingdom

  • *hasan.sadat@lrz.uni-muenchen.de

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Vol. 81, Iss. 21 — 1 June 2010

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