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Determination of cation distribution in Ti4+ and Co2+ substituted barium ferrite by Mössbauer spectroscopy

Abstract

In barium ferrite, BaFe12O19, the Fe3+ ions were gradually substituted by Ti4+ and Co2+. The cation distribution of the various lattice sites is determined as a function of the degree of replacement. The preferred site population is discussed by a substitution model.

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Kreber, E., Gonser, U. Determination of cation distribution in Ti4+ and Co2+ substituted barium ferrite by Mössbauer spectroscopy. Appl. Phys. 10, 175–180 (1976). https://doi.org/10.1007/BF00896336

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PACS Code

  • 75.30
  • 76