Mechanism of the Verwey transition in magnetite
arXiv:cond-mat/0610363 · doi:10.1103/PhysRevLett.97.156402
Abstract
By combining {\it ab initio} results for the electronic structure and phonon spectrum with the group theory, we establish the origin of the Verwey transition in FeO. Two primary order parameters with and symmetries are identified. They induce the phase transformation from the high-temperature cubic to the low-temperature monoclinic structure. The on-site Coulomb interaction 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. {\it Published in Phys. Rev. Lett. {\bf 97}, 156402 (2006).}
arXiv comment5 pages, 3 figures
References in corpus (6)
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- Charge and orbital order in Fe_3O_4
- Resonant X-ray diffraction studies on the charge ordering in magnetite
- High-energy photoemission on Fe3O4: Small polaron physics and the Verwey transition
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