Abstract

Experimental data on the temperature dependences of the magnetization of manganites, cobaltites, and ferrites are analyzed. Their common feature is magnetization irreversibility: below a temperature T* for a fixed field strength, the magnetization is different for cooling in a field (MFC) and in zero field (MZFC). It is shown that the T*(H) curve is universal for all the dispersed oxides (nanocompound, nanopowder) and is consistent with the theoretical Almeida-Thouless curve (T* ∼ H2/3) over the entire range of magnetic fields. In the case of monolithic samples (single crystals, ceramics), in strong magnetic fields there is a transition to a quadratic dependence T* ∼ H2 in agreement with the Gabay-Toulousse theory. This phenomenon is interpreted in terms of spin-glass polyamorphism.

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