论文标题

磁性各向异性SRRUO3膜中的各向同性轨道磁矩

Isotropic orbital magnetic moments in magnetically anisotropic SrRuO3 films

论文作者

Wakabayashi, Yuki K., Kobayashi, Masaki, Takeda, Yukiharu, Kitamura, Miho, Takeda, Takahito, Okano, Ryo, Krockenberger, Yoshiharu, Taniyasu, Yoshitaka, Yamamoto, Hideki

论文摘要

外延紧张的SRRRUO3膜已成为理解金属氧化物中磁各向异性的模型系统。在本文中,我们使用高质量的外延紧张(压缩和拉伸)SRRUO3膜研究了RU 4D和O 2P电子结构和磁性的各向异性。 RU 4D和O 2P轨道之间的元素特异性磁性和杂交的特征是RU M2,3-边缘和O K边缘软X射线吸收光谱和X射线磁性圆形二分法测量。 RU 4D和O 2P磁矩的磁化曲线是相同的,无论应变类型如何,表明RU和O离子之间的强磁耦合。尽管在压缩和抗拉伸质量的SRRRUO3膜中具有垂直和平面磁各向异性,但相对于自旋磁矩的电子结构和轨道磁矩相对于自旋磁矩还是各向同性的。即,轨道磁矩对磁各向异性的贡献很小。该结果与Bruno模型相矛盾,Bruno模型是磁各向异性源于垂直方向和平面方向之间轨道磁矩的差异。还讨论了应变诱导的四极杆矩对磁各向异性的贡献。

Epitaxially strained SrRuO3 films have been a model system for understanding the magnetic anisotropy in metallic oxides. In this paper, we investigate the anisotropy of the Ru 4d and O 2p electronic structure and magnetic properties using high-quality epitaxially strained (compressive and tensile) SrRuO3 films grown by machine-learning-assisted molecular beam epitaxy. The element-specific magnetic properties and the hybridization between the Ru 4d and O 2p orbitals were characterized by Ru M2,3-edge and O K-edge soft X-ray absorption spectroscopy and X-ray magnetic circular dichroism measurements. The magnetization curves for the Ru 4d and O 2p magnetic moments are identical, irrespective of the strain type, indicating the strong magnetic coupling between the Ru and O ions. The electronic structure and the orbital magnetic moment relative to the spin magnetic moment are isotropic despite the perpendicular and in-plane magnetic anisotropy in the compressive-strained and tensile-strained SrRuO3 films; i.e., the orbital magnetic moments have a negligibly small contribution to the magnetic anisotropy. This result contradicts Bruno model, where magnetic anisotropy arises from the difference in the orbital magnetic moment between the perpendicular and in-plane directions. Contributions of strain-induced electric quadrupole moments to the magnetic anisotropy are discussed, too.

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