Abstract
A neutron diffraction investigation revealed that the degree of inversiony in quenched samples of MnFe2O4 varied from 0·06 for samples annealed at 330 °C to a constant value 0·22 for samples annealed at 600 °C and higher temperatures. On the other ahnd, measurements on samples at elevated temperatures showed further increase ofy above 600 °C. The reversibility of the temperature changes ofy was confirmed.
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The authors express their thanks to Dr. Z.Šimša for stimulating discussions.
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Jirák, Z., Vratislav, S. Temperature dependence of distribution of cations in MnFe2O4 . Czech J Phys 24, 642–647 (1974). https://doi.org/10.1007/BF01587300
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DOI: https://doi.org/10.1007/BF01587300