Author： Aliev Sh. M. Kamilov I. K. Guseinov M. M. Shakhshaev Sh. O. Abduev A. Kh.
Publisher： Springer Publishing Company
ISSN： 1064-8887
Source： Russian Physics Journal, Vol.47, Iss.2, 2004-02, pp. : 189-193
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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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