摘要
详细研究了Dy2(Fe1-xSix)17(x=0,004,008,012,016,020)系列化合物的晶格结构和内禀磁性。X射线衍射分析表明,Dy2(Fe1-xSix)17系列化合物呈现Th2Ni17结构相或Th2Zn17结构相,居里温度TC随x的增大而增大,饱和磁化强度σs随x的增加而减小。由穆斯堡尔谱分析得到,各Fe晶位的超精细场随x的增加而减小。但4f哑铃位减小最快。由实验结果可以看到。
The crystal and magenetic properties of Dy 2(Fe 1- x Si x ) 17 with x equal to 0 0, 0 04, 0 08, 0 10, 0 12, 0 16, 0 20 have been investigated with X ray diffraction and 57 Fe Mssbauer effects methods. They crystallize in the hexagonal Th 2Ni 17 type structure or Th 2Zn 17 type structure. With the increase of Si content, their curie temperatures increase, while their saturation magnetizations decrease. From the Mssbauer spectra data., it is found that the hyperfine field in all Fe crystal sites is weakened with Si content increasing and the 4f dumbell site decrease fastestly. From the experimental results, it can be seen that the effects of substituing Si for Fe is active.
出处
《中国稀土学报》
CAS
CSCD
北大核心
1997年第1期22-26,共5页
Journal of the Chinese Society of Rare Earths
关键词
镝
穆斯堡尔效应
平均铁磁矩
稀土族元素
Rare earth, R 2Fe 17 compounds, Substitutional atom, Mssbauer effects, Hyperfine field, Average Fe magnetic moment