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

Nature volume 144, pages 327–328 (1939) Cite this article

Abstract

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:

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References

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Authors and Affiliations

  1. Natuurkundig Laboratorium, N. V. Philips’ Gloeilampenfabrieken, Eindhoven
    E. J. W. VERWEY

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VERWEY, E. Electronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low Temperatures.Nature 144, 327–328 (1939). https://doi.org/10.1038/144327b0

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