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Magnetic ordering in rare earth metal dysprosium revealed by neutron diffraction studies in a large-volume diamond anvil cell

机译:稀土金属镝中的磁性排序由中子衍射研究中的大容量金刚石砧座细胞

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摘要

A high pressure low-temperature neutron diffraction study has been carried out on rare earth metal Dysprosium (Dy) to 10.8 GPa and 8 K in a large-volume diamond anvil cell using a spallation neutron source. Dy crystallizes in an ambient pressure hexagonal close packed phase and forms an incommensurate helical antiferromagnetic phase, marked by the appearance of superlattice magnetic peaks below 176 K with a turn-angle between the hexagonal layers that increases both with increasing temperature and pressure. The ferromagnetic transition below 87 K is marked by an increase in intensity of nuclear peaks with disappearance of magnetic superlattice reflections. Dy transforms to an alpha-Samarium (α-Sm) phase at 7 GPa and only ferromagnetic ordering is observed for this high pressure phase. The ferromagnetic transition is observed at 59 K in the α-Sm phase at 10.8 GPa in close agreement with the magnetic ordering temperature obtained from electrical transport measurements. In the entire pressuretemperature range of this study, Dy shows a negative thermal expansion coefficient of as much as -2.5% in the magnetically ordered phases between 200 and 8 K.
机译:使用介质中子源在大容量金刚石砧座中,在稀土金属镝(Dy)至10k和8k中,在大容量金刚石砧座中进行了高压低温中子衍射研究。 Dy在环境压力六边形紧密填充相中结晶并形成所联素螺旋反铁磁相,通过低于176k的超晶格磁峰的外观,其六边形层之间的转角随着温度和压力而增加而增加。在87 k以下的铁磁性过渡标志着磁性超晶格反射消失的核峰强度的增加。 Dy在7GPa下转化为α-钐(α-SM)相,并且仅观察到该高压相的铁磁性排序。在10.8GPa的α-Sm相中观察到铁磁性转变在10.8GPa的α-SM相中,与电气传输测量获得的磁性有序温度紧密一致。在本研究的整个压力测量范围内,DY在200至8K之间的磁性有序相中显示出负热膨胀系数的负热膨胀系数高达-2.5%。

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