Mechanism of the Verwey Transition in Magnetite

Przemysław Piekarz, Krzysztof Parlinski, and Andrzej M. Oleś
Phys. Rev. Lett. 97, 156402 – Published 12 October 2006

Abstract

By combining ab initio results for the electronic structure and phonon spectrum with the group theory, we establish the origin of the Verwey transition in Fe3O4. Two primary order parameters with X3 and Δ5 symmetries are identified. They induce the phase transformation from the high-temperature cubic to the low-temperature monoclinic structure. The on-site Coulomb interaction U between 3d electrons at Fe ions plays a crucial role in this transition—it amplifies the coupling of phonons to conduction electrons and thus opens a gap at the Fermi energy.

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  • Received 14 June 2006

DOI:https://doi.org/10.1103/PhysRevLett.97.156402

©2006 American Physical Society

Authors & Affiliations

Przemysław Piekarz1, Krzysztof Parlinski1, and Andrzej M. Oleś1,2

  • 1Institute of Nuclear Physics, Polish Academy of Sciences, Radzikowskiego 152, PL-31342 Kraków, Poland
  • 2Max-Planck-Institut für Festkörperforschung, Heisenbergstrasse 1, D-70569 Stuttgart, Germany

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Issue

Vol. 97, Iss. 15 — 13 October 2006

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