Abstract

The atomic structure at the Fe 3O 4–MgO interface and its role in defining magnetic behaviour in Fe 3O 4–MgO multilayers, grown by MBE on MgO(001), has recently been a subject of much interest and controversy: the existence of a “dead” magnetic layer at the interface has been proposed to explain why ultra-thin magnetite layers become nonmagnetic. By using Mössbauer probe layers it was shown that this model is incorrect. In this paper we present additional structural evidence, from X-ray reflectivity and RHEED measurements, showing that the magnetite layers have the same structure and composition at the interface and in the bulk in agreement with a uniform magnetic structure throughout the entire layer.

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