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On the cation distribution in the spinel systemyMg2TiO4−(1−y)MgFe2O4

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Abstract

The cation distribution and the oxygen parameter for the system Mg1+y Fe2(1−y) Ti y O4 have been determined using the intensities of X-ray reflections. Results are given for slowly cooled and quanched samples. An explanation is proposed to account for the behaviour of the lattice parameter and the oxygen parameter.

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Authors and Affiliations

  1. Laboratory for Magnetism, University of Ghent, Proeftuinstraat, 86, B-9000, Ghent, Belgium

    E. De Grave, J. De Sitter & R. Vandenberghe

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  1. E. De Grave
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  2. J. De Sitter
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  3. R. Vandenberghe
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De Grave, E., De Sitter, J. & Vandenberghe, R. On the cation distribution in the spinel systemyMg2TiO4−(1−y)MgFe2O4 . Appl. Phys. 7, 77–80 (1975). https://doi.org/10.1007/BF00900525

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  • DOI: https://doi.org/10.1007/BF00900525

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