希土類元素置換で酸化鉄(黒さび)の磁化増大に成功~ありふれた磁石の性能向上のためのデザイン則を実証~

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2025-03-03 東京大学

東京大学大学院工学系研究科の研究グループは、マグネタイト(Fe₃O₄)に希土類元素であるユウロピウム(Eu)を添加することで、飽和磁化の増大に成功しました。成膜速度を調整してEuの結晶内分布を制御し、正四面体サイトの鉄(Fe)をEuで置換した薄膜において、磁化が増大することを確認しました。さらに、軟X線内殻吸収磁気円二色性(XMCD)実験により、EuとFeの電子スピンが強磁性的に結合していることが明らかになりました。

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Fe3O4の飽和磁化を高めるサイト選択的希土類置換によって誘起される非平行磁性 Noncollinear Magnetism in Fe3O4 Induced via Site-Selective Rare-Earth Substitution Boosting Its Saturation Magnetization

Haining Li, Masaki Kobayashi, Sonju Kou, Md Shamim Sarker, E M K Ikball Ahamed, Kohei Yamagami, Tetsuya Fukushima, Kaijie Ma, Shuting Ma, Takahito Takeda, Ryo Okano …
Small  Published: 24 February 2025
DOI:https://doi.org/10.1002/smll.202411133

希土類元素置換で酸化鉄(黒さび)の磁化増大に成功~ありふれた磁石の性能向上のためのデザイン則を実証~

Abstract

Substituting rare-earth Eu ions with a large atomic number into 3d transition metal oxides can precisely control their magnetic properties through significant spin-orbit coupling, leading to noncollinear magnetism. Experimental investigations are combined with density functional theory to explore site-selective Eu3+ substitution as a strategy to enhance the magnetic properties of Fe3O4 thin films. The substitution location of Eu3+, that is, octahedral versus tetrahedral, is confirmed by electrical resistivities and valence band photoemission measurements. Tetrahedrally Eu-substituted Fe3O4 exhibited an exceptionally enhanced saturation magnetization MS of up to 4.4 μB/f.u. because of noncollinearity, whereas octahedrally Eu-substituted Fe3O4 showed significantly reduced MS. X-ray absorption spectroscopy and X-ray magnetic circular dichroism measurements clearly revealed that in the tetrahedrally Eu-substituted Fe3O4, the Eu3+ magnetic moment positively contributed to the orbital magnetic moment that exhibited strong magnetic anisotropy. The deviation of the observed MS from the lower value predicted by Néel’s theory of collinear ferrimagnetism further supported the role of noncollinearity. These results provide empirical evidence for the spin configuration of tetrahedrally Eu-substituted Fe3O4 and a new perspective for designing practical ferrimagnetic 4f compounds with exceptional MS.

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