arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2007.12024cond-mat.mtrl-scicond-mat.str-el
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黄钾铁矾中磁序的压力诱导崩塌

Pressure induced collapse of magnetic order in jarosite

Ryan A. Klein, James P. S. Walsh, Samantha M. Clarke, Zhenxian Liu, E. Ercan Alp, Wenli Bi, Yue Meng, Alison B. Altman, Paul Chow, Yuming Xiao, M. R. Norman, Ja… 展开作者

Ryan A. Klein, James P. S. Walsh, Samantha M. Clarke, Zhenxian Liu, E. Ercan Alp, Wenli Bi, Yue Meng, Alison B. Altman, Paul Chow, Yuming Xiao, M. R. Norman, James M. Rondinelli, Steven D. Jacobsen, Danilo Puggioni, Danna E. Freedman

摘要:

我们报道了在~45 GPa压力下,受抑的Kagomé材料黄钾铁矾发生了压力诱导的相变,导致磁序消失.使用一套实验技术,我们的特点是通过这种相变的黄钾铁矾的结构,电子和磁性的变化。同步辐射粉末X射线衍射和傅里叶变换红外光谱实验,结合密度泛函理论计算结果进行分析,表明该材料从R-3 m结构转变为具有R-3c空间群的结构。由此产生的相具有罕见的扭曲的kagomé晶格,其中等边Fe 3+三角形的完整性持续存在。基于对称性的论点,我们假设,由此产生的结构变化改变磁相互作用,有利于在高压下可能的量子顺磁相。

英文摘要:

We report a pressure-induced phase transition in the frustrated kagomé material jarosite at ~45 GPa, which leads to the disappearance of magnetic order. Using a suite of experimental techniques, we characterize the structural, electronic, and magnetic changes in jarosite through this phase transition. Synchrotron powder X-ray diffraction and Fourier transform infrared spectroscopy experiments, analyzed in aggregate with the results from density functional theory calculations, indicate that the material changes from a R-3m structure to a structure with a R-3c space group. The resulting phase features a rare twisted kagomé lattice in which the integrity of the equilateral Fe3+ triangles persists. Based on symmetry arguments we hypothesize that the resulting structural changes alter the magnetic interactions to favor a possible quantum paramagnetic phase at high pressure.

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