U(Mn1−xFex)2Si2的晶体和磁性能

J.J Bara, H.U Hrynkiewicz, A Szytuta
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引用次数: 3

摘要

通过直接熔融UMn2Si2和UFe2Si2组分,合成了固溶体系统U(Mn1−xFex)2Si2(0⩽x \108777 1),并用x射线衍射、磁强计和穆斯堡尔效应等方法进行了研究。所研究的系列在许多方面与其他元素形成的同构系列表现相似。晶格常数的值服从维加定律。异构体位移和四极分裂在铁浓度范围内逐渐变化。四极分裂反映了与铁位点邻居的理想四面体配位的偏差。富含锰的样品(x⩽0.3)在78 K时被发现是铁磁体,而其他样品在78 K以上表现为泡利顺磁体。居里温度和超精细磁场随着铁浓度的增加而强烈降低。居里温度的组分依赖性由海森堡模型很好地描述,其中考虑了最近邻居之间的磁相互作用和单轴磁各向异性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Crystal and magnetic properties of U(Mn1−xFex)2Si2

The solid solution system U(Mn1−xFex)2Si2 (0 ⩽ x ⩽ 1) was synthesized by direct melting of the UMn2Si2 and UFe2Si2 components and investigated by X-ray diffraction, magnetometric and Mössbauer effect methods. The series investigated behaves similarly in many respects to the isostructural ones formed with other elements. The values of the lattice constants obey Vegard's law. The isomer shift and quadrupole splitting vary gradually across the range of iron concentration. The quadrupole splitting reflects a deviation from the ideal tetrahedral coordination of iron site neighbours. The manganese-rich samples (x ⩽ 0.3) were found to be ferromagnets at 78 K while the others behave as Pauli paramagnets above 78 K. The Curie temperature and hyperfine magnetic field decrease strongly with increasing iron concentration. The composition dependence of the Curie temperature is well described by the Heisenberg model in which the magnetic interactions between nearest neighbours and the uniaxial magnetic anisotropy were taken into account.

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