Electronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low Temperatures (original) (raw)
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- Published: 19 August 1939
Nature volume 144, pages 327–328 (1939) Cite this article
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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
- Verwey, E. J. W., and de Boer, J. H., Rec. Trav. chim., 55, 531 (1936); de Boer, J. H., and Verwey, E. J. W., Proc. Phys. Soc., 49, extra part, 57 (1937); Schottky, W., Z. tech. Phys., 19, 611 (1938).
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Authors and Affiliations
- 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
- Issue date: 19 August 1939
- DOI: https://doi.org/10.1038/144327b0