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基于 U 的铁磁体磁各向异性性质的巡游-局域化二分性。

Itinerant-localized dichotomy in magnetic anisotropic properties of U-based ferromagnets.

机构信息

Institute of Physics, Czech Academy of Sciences, Na Slovance 2, 18221, Prague, Czech Republic.

Department of Molecular Chemistry and Materials Science, Weizmann Institute of Science, 76100, Rehovoth, Israel.

出版信息

Sci Rep. 2023 Feb 14;13(1):2646. doi: 10.1038/s41598-023-29823-2.

Abstract

The electronic structure, spin and orbital magnetic moments, and the magnetic anisotropy energy in selected U-based compounds are investigated making use of the correlated band theory. First, we demonstrate that the LSDA+U approach with exact atomic limit implemented as a combination of the relativistic density functional theory with the Anderson impurity model provides a good quantitative description for UGa[Formula: see text]. Further, the method is applied to UFe[Formula: see text] and UFe[Formula: see text]Si[Formula: see text] ferromagnets. The calculated positive uniaxial magnetic anisotropy together with negative enthalpy of formation for UFe[Formula: see text]Si[Formula: see text] make it as a candidate for the magnetically hard materials. Our studies suggest a viable route for further development of the rare-earth-lean permanent magnets by replacing a part of U atoms by some rare-earth like Sm in UFe[Formula: see text]Si[Formula: see text].

摘要

利用相关能带理论,研究了选定的 U 基化合物的电子结构、自旋和轨道磁矩以及磁各向异性能。首先,我们证明了 LSDA+U 方法与精确原子极限的结合,即相对论密度泛函理论与安德森杂质模型的组合,为 UGa[Formula: see text]提供了良好的定量描述。此外,该方法还应用于 UFe[Formula: see text]和 UFe[Formula: see text]Si[Formula: see text]铁磁体。计算出的正单轴各向异性磁矩与 UFe[Formula: see text]Si[Formula: see text]的负形成焓使它成为磁性硬材料的候选材料。我们的研究表明,通过在 UFe[Formula: see text]Si[Formula: see text]中用部分类似于 Sm 的稀土元素替代部分 U 原子,可以为开发稀土贫永磁体提供可行的途径。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/f1c8/9929282/f5181f537a42/41598_2023_29823_Fig1_HTML.jpg

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