Magnetic Neutron Scattering from the Rare-Earth Intermetallic Compound System R3Pd20Si6 (R = Rare Earth)
Magnetic Neutron Scattering from the Rare-Earth Intermetallic Compound System R3Pd20Si6 (R = Rare Earth)
复制标题
稀土金属间化合物体系 R3Pd20Si6（R = 稀土）的磁中子散射
DOI：
10.4028/www.scientific.net/msf.443-444.233
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发表时间：
2004
期刊：
影响因子：
--
通讯作者：
H. Kitazawa
中科院分区：
文献类型：
--
作者：
T. Herrmannsdörfer;A. Dönni;P. Fischer;L. Keller;S. Janssen;A. Furrer;B. van den Brandt;H. Kitazawa
用弹性和非弹性中子散射方法研究了稀土金属间化合物R3 Pd_（20）Si_6（R =稀土）的低温磁性。由于在立方晶体结构（空间群Fm-3 m）中从4a和8 c位置构建的两个稀土亚晶格，化合物显示出具有两个不同传播矢量的连续磁有序。在这份报告中，我们给出了在3-20-6-系统的磁结构和晶体电场的结果的概述。
The low-temperature magnetic properties of the rare-earth intermetallic compound system R3Pd20Si6 (R = rare earth) were studied by elastic and inelastic neutron scattering. The compounds show due to the two rare-earth sublattices built from the 4a and 8c sites in the cubic crystal structure (space group Fm-3m) successive magnetic ordering with two different propagation vectors. In this report, we give an overview of the results obtained for the magnetic structures and the crystalline electric fields in the 3-20-6-system.