Abstract
It is demonstrated by the Mössbauer spectroscopy method that the residual magnetizations of ferrite-gadolinium garnet sublattices anomalously increase near the compensation temperature. Anomalies for a single-crystal sample are observed in a narrower temperature interval than for a polycrystalline sample. The detected phenomenon is explained by the rearrangement of the ferrite domain structure near the compensation temperature.
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Aliev, S.M., Kamilov, I.K., Guseinov, M.M. et al. Behavior of the Residual Magnetizations of Ferrite-Gadolinium Garnet Sublattices near the Compensation Temperature. Russian Physics Journal 47, 189–193 (2004). https://doi.org/10.1023/B:RUPJ.0000034487.47559.1d
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DOI: https://doi.org/10.1023/B:RUPJ.0000034487.47559.1d