Crystal structure and magnetic properties of R(2) (Fe, M)(17+delta)

被引:3
作者
Hasebe, A
Otsuki, E
机构
[1] Materials Development Laboratory, Tokin Corporation, Taihaku-ku, 982, Sendai
来源
MATERIALS TRANSACTIONS JIM | 1996年 / 37卷 / 04期
关键词
rare earth-transition metal compound; magnetic properties; Curie temperature; saturation magnetization; crystal structure; rare earth permanent magnet;
D O I
10.2320/matertrans1989.37.870
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We discovered a novel compound expressed by R(2)(Fe, M)(17+delta) in the compositional range between 2-17 and 1-12. Hong-Shou Li et al. reported R(2)(Fe, M)(29) which is stoichiometric compound with monoclinic structure. These compounds show similar X-ray diffraction patterns. In this paper, syntheses of R(2)(Fe, M)(17+delta) were attempted for various rare earth elements, R and transition metals, M, and their crystal structure and magnetic properties were investigated. It was found that nonstoichiometric compound, R(2)(Fe, M)(17+delta) (delta=1.0-4.0) forms for R=Ce,Nd,Sm,Gd,Dy,Y and M=Ti,V,Mo,W. X-ray and electron beam diffraction analyses revealed that the compound has hexagonal structure with the space group of <P(6)over bar>2m. The nonstoichiometry of the compound can be attributed to the diversity in the atom orders in the c-planes. The saturation magnetization of R(2)(Fe,M)(17+delta) is independent of the kind of M-metals, however curie temperature changes as 315K(Mo), 333K(Ti), 342K(W) and 390K(V), which is similar tendency to R(Fe,M)(32) compounds. For R(2)(Fe,M)(17+delta) the saturation magnetization and curie temperature show a maximum value for Nd(126 x 10(-6)Wb . mkg(-1)) and Gd(541K) in the rare earth series, respectively.
引用
收藏
页码:870 / 877
页数:8
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