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Low Temperature Properties of Selected Kramers Rare Earth Oxychlorides.

机译:所选克拉姆斯稀土氧化氯化物的低温性能。

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In this work, we present low temperature magnetic and electronic properties measured on selected Kramers rare-earth oxychlorides REOCl, RE= Nd, Gd, Dy which adopt the PbFCl-type of structure. Prepared powder samples were characterized by means of standard structural, magnetic and electronic methods as X-ray diffraction (300 K), heat capacity (0.3 K - 12 K) and susceptibility measurements (2 K - 300 K, at ambient pressure and hydrostatic pressures up to 0.68 ± 0.01 GPa). Our results indicate new transition to the ordered magnetic state for GdOCl and NdOCl compound at temperatures of 5 K and 1.5 K, respectively. We found small increase of magnetization saturation value of dysprosium oxychloride with an applied hydrostatic pressure, but no remarkable changes occur to antiferromagnetic transition temperature (TN ~ 9.2 K) when a moderate hydrostatic pressure (p ≤ 0.68 ± 0.01 GPa) was applied. Observed deviations from the Curie Weiss behavior below 26 K can be caused by the vicinity of the magnetic ordering temperature, or another magnetic effects. The single crystal experiments which will solve this opened question are in progress.
机译:在这项工作中,在选定克拉默斯稀土氯氧化物REOCl,RE =钕,钆,镝,其采用PbFCl型结构的测量,我们本发明的低温磁性和电子性质。和磁化率测量(2 k - 制备的粉末样品通过的标准结构,磁和电子方法如X射线衍射(300 K),热容量(12K个0.3 K) - 的装置,其特征在于300°K,在环境压力和流体静压力高达0.68±0.01 GPa)的。我们的结果表明在分别5 K和1.5 K,的温度下的新过渡到GdOCl和NdOCl化合物有序磁状态。我们发现镝酰氯磁化饱和值的小的增加与施加的流体静压力,但发生在施加适度的流体静压(P≤0.68±0.01 GPa)的反铁磁性转变温度(TN〜9.2 K)没有显着的变化。从下面26 k中的居里魏斯行为观察到的偏差可以通过磁有序温度附近,或其它磁效应引起的。单晶的实验,这将解决这个问题,打开正在进行中。

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