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四方晶体稀土-铁-硼系金属间化合物的结构和磁性

STRUCTURAL AND MAGNETIC PROPERTIES OF THE TETRAGONAL RARE EARTHIRON-BORON COMPOUNDS

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【作者】 杨应昌何文望陈海英邢峰兰健

【Author】 Yang Yingchang, Ho Wenwang, Chen Haiying, Xing Feng, Lan Jian (Peking University)

【机构】 北京大学北京大学

【摘要】 用磁测量和X射线衍射方法研究了R15B7Fe78(R=MM,Pr,Nd,Sm,Gd,Y)和Nd15B7(Fe1-xMx)78(M=Co,Mn,Cr)的结构和内禀磁性。X射线衍射实验表明,这些化合物皆属四方结构。R15B7Fe28的晶格常数随稀土原子序数的增加而减小,反映了镧系收缩的特点。居里温度随稀土金属原子序数的增加而增高,反映了稀土-铁原子间的间接交换作用的影响,Gd15B7Fe78具有最高的居里温度。在Nd15B7(Fe1-xMz)78中,以Co代Fe时,晶格常数随x的增加而减小;居里温度随x的增加而单调显著上升。以Mn代Fe时,晶格常数随x的增加而增大;居里温度则随x的增加而急剧下降。居里温度的变化,说明R15B7Fe78的居里温度主要由3d过渡族原子间的直接交换作用所决定的。以Co代Fe,当x=0.2时,Nd15B7(Fe1-xCox)78的饱和磁化强度出现极值。

【Abstract】 The crystallographic structure and intrinsic magnetic properties of R15 B7 Fe78(R=MM, Pr, Nd, Sm, Gd and Y) and Nd15B7(Fe1-xMx)78(M=Co, Mn and Cr) have been studied by magnetic measurements and X-ray diffraction experiments. These compounds crystallize in a tetragonal structure. The Lanthanide contraction results in a decrease of lattice parameters with increasing atomic number of rare earth elements. The curie temperature Tc is found to be increased with increasing atomic number of R, and Tc of Gd15B7Fe78 is the highest, which shows the effect of R-Fe exchange interaction. For the series of Nd15B7(Fe1-xMx)78, curie temperature Tc increases significantly with the content of Co, whereas the substitution of Fe with Mn results in a sharp decrease of curie temperature. The sensitive effect of substitution of Fe with other 3d-transition metals on curie temperature indicates that the curie temperature of R15B7Fe78 is essentialy determined by 3d-3d atoms exchange interaction. The variation of saturation magnetization of Nd15B7(Fe1-xCox)78 as a function of the content x of Co shows a maximum around x=0.2.

  • 【文献出处】 中国稀土学报 ,Journal of The Chinese Rare Earth Society , 编辑部邮箱 ,1985年02期
  • 【被引频次】4
  • 【下载频次】84
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