Thin films of dilute magnetic oxides often exhibit high-temperature ferromagnetism with magnetization curves of the form M ¿ Mstanh (H/H0); the curves are practically anhysteretic and temperature-independent below room temperature. The absence of temperature-dependent coercivity indicates that the magnetization process is dominated by magnetic dipole interactions, not by magnetocrystalline anisotropy. In a model of ferromagnetic grain boundaries, H0¿ 0.14M0, where M0is the magnetization of the ferromagnetic regions. Quantitative analysis of more than 200 films of different oxides reveals that only a few percent of the volume of these films is magnetically ordered.
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Coey et al. (2010) studied this question.
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