Annotation
Self-reversal of thermal magnetization in natural ferrite (a solid solution of the magnetite and maghemite with Curie temperature of 595°C) was studied. The experimental results show that self-reversal occurs as a result of the effect of negative exchange anisotropy in the vicinity of the Curie temperature via a mechanism related to the presence of a weak magnetic sublattice in ferrite.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
V.I. Trukhin, V.I. Maksimochkin, Yu.A. Elesin, V.A. Zhilyaeva
Department of Physics of Earth, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Department of Physics of Earth, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
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