Origin of Perpendicular Magnetic Anisotropy in CoxFe3-xO4+δ Thin Films Studied by X-ray Magnetic Circular and Linear Dichroisms

Abstract

We investigate the element-specific spin and orbital states and their roles on magnetic anisotropy in the Co-ferrite (CoxFe3-xO4+δ (001)) thin films which exhibit perpendicular magnetic anisotropy (PMA). The origin of PMA in the low x region (x < 1) can be mainly explained by the large perpendicular orbital magnetic moments in the Co2+ (3d7) states detected by X-ray magnetic circular and linear dichroisms (XMCD/XMLD). The XMLD for a PMA film (x=0.2) with square hysteresis curve shows the oblate charge distribution in the Co2+ site, which is consistent with the change in local nearest neighbor distance in Co detected by extended X-ray absorption fine structure analysis. Our finding reveals that the microscopic origin of PMA in Co-ferrite comes from the enhanced orbital magnetic moments along out-of-plane [001] direction through in-plane charge distribution by tensile strain, which adds the material functionalities in spinel ferrite thin films from the viewpoint of strain and orbital magnetic moments.

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