Electronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low Temperatures

@article{Verwey1939ElectronicCO,
  title={Electronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low Temperatures},
  author={E. J. W. Verwey},
  journal={Nature},
  year={1939},
  volume={144},
  pages={327-328}
}
  • E. Verwey
  • Published 1 August 1939
  • Materials Science
  • Nature
WE have measured the electronic conductivity, down to liquid nitrogen temperature, of a number of iron oxides of the homogeneous ‘Fe3O4’ phase, especially as a function of the exact stoichiometrie composition of the material. This seemed of theoretical interest for several reasons: 
Ultralow Thermal Conductivity in Nanoporous Crystalline Fe3O4
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Cation, magnetic, and charge ordering in MnFe3O5† †Electronic supplementary information (ESI) available: Tables of crystallographic results and powder synchrotron profile fit. See DOI: 10.1039/c8tc00053k
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Link between Magnetic and Dielectric Properties in Magnetite
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Non-collinear Magnetic Structure on the Fe3O4(111) Surface
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The Crystal Structure of γ-Fe2O3 and γ-Al2O3
\. The oxides Fe203 and Al203 are known to crystallize in different modifications. The stable oxides are a-Fe203 (haematite) and a-Al2()3 (corundum); they form structures of the same type with
Crystal Structures and Expansion Anomalies of MnO, MnS, FeO, Fe3O4 Between 100°K and 200°K
(1) Determinations have been made of structure type and lattice constants of MnO, MnS, FeO and Fe3O4 at temperatures near those at which these substances show specific heat anomalies. (2) No major