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Neutron diffraction study of magnetic ordering in high pressure phases of rare earth metal holmium

机译:稀土金属钬高压阶段磁性排序中子衍射研究

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摘要

The magnetic ordering in rare earth metals is well established for ambient pressure crystal structures, however, little is known about the magnetic ordering in their corresponding high-pressure crystalline modifications. Holmium (Ho) was studied in a large-volume diamond anvil cell at the Spallation Neutron Source to high-pressure up to 20 GPa and to low-temperature to 10 K. We have conducted two independent high-pressure low-temperature experiments under non-hydrostatic and quasi-hydrostatic pressure conditions respectively. The ambient pressure hexagonal close packed (hcp) phase of holmium shows two magnetic transitions below 10 GPa one to an incommensurate Antiferromagnetic (AFM) phase and another to a conical-Ferromagnetic (c-FM) phase. In contrast, alpha-Samarium-type (α-Sm) phase above 10 GPa and the double hexagonal close packed (dhcp) phase above 19 GPa show only one FM transition marked by the appearance of a magnetic peak at 3 A and the concurrent enhancement of nuclear peaks below 30 K. These new transitions observed by neutron diffraction can be accounted by a commensurate superlattice formation along c-axis in both the α-Sm-type phase and the dhcp phase.
机译:对于环境压力晶体结构,稀土金属中的磁性排序很好地确定,关于它们相应的高压晶体修饰中的磁性排序很少。在初级金刚石砧座上研究了钬(HO),在初步的中子源上至高达20GPa的高压和低温至10k。我们已经在非中间进行了两个独立的高压低温实验 - 水滴分别和准静水压力条件。钬的环境压力六方密切填充(HCP)相位显示出低于10GPa的两个磁性转变为10GPa,给中链反铁磁性(AFM)相,另一个至锥形铁磁性(C-FM)相。相反,在10GPa的α-钐型(α-SM)相和高于19GPa的双六边形关闭填充(DHCP)相位,仅显示通过3A和并发增强的磁峰的外观标记的一个FM过渡在30k以下的核峰值中。通过中子衍射观察的这些新的转变可以通过α-SM型相和DHCP相中沿C轴的相称超晶格形成来抵押。

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