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Is the Verwey transition in Fe(3)O(4) magnetite driven by a Peierls distortion?

作者信息

Shchennikov Vladimir V, Ovsyannikov Sergey V

机构信息

High Pressure Group, Institute of Metal Physics, Russian Academy of Sciences, Urals Division, GSP-170, 18 S Kovalevskaya Street, Yekaterinburg 620041, Russia.

出版信息

J Phys Condens Matter. 2009 Jul 8;21(27):271001. doi: 10.1088/0953-8984/21/27/271001. Epub 2009 Jun 12.

DOI:10.1088/0953-8984/21/27/271001
PMID:21828481
Abstract

In this viewpoint article we analyse recent crucial structural, optical and transport experiments on Fe(3)O(4) magnetite across the Verwey transition at T(V)∼120-125 K. We find that all the relevant experimental data are consistent with a model of a Peierls distortion in the cubic spinel lattice, and likewise, some of them evidence against the original and still distributed hypothesis of the long range charge ordering origin of the Verwey transition. An estimated Peierls transition temperature (T(P)) is comparable with T(V). The Peierls model provides new insight into the electronic properties of magnetite. Application of the Peierls model to some other systems is briefly discussed also.

摘要

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