The properties of a magnetically ordered buried Fe oxide layer are presented. This oxide has a room-temperature magnetization exceeding that of Fe₃O₄ by 42% and of γ-Fe₂O₃ by 89%. The oxide consists of a component (70%) with a net moment of 2.0μB/Fe ion, while the remaining spins yield no net moment. The oxide magnetization is stabilized in part by the proximate Fe metal.
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Beach et al. (2003) studied this question.
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