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从量子无序到 s=1/2 kagome 晶格中的磁有序:高压下水镁石的结构和磁性研究。

From quantum disorder to magnetic order in an s=1/2 kagome lattice: a structural and magnetic study of herbertsmithite at high pressure.

机构信息

Frank Laboratory of Neutron Physics, Joint Institute for Nuclear Research, 141980 Dubna, Russia.

出版信息

Phys Rev Lett. 2012 May 4;108(18):187207. doi: 10.1103/PhysRevLett.108.187207. Epub 2012 May 3.

Abstract

The structural and magnetic properties of deuterated herbertsmithite have been studied by means of neutron powder diffraction and magnetic susceptibility measurements in a wide range of temperatures and pressures. The experimental data demonstrate that a phase transition from the quantum-disordered spin-liquid phase to the long-range ordered antiferromagnetic phase with the Néel temperature T(N)=6  K is induced at P=2.5  GPa. The observed decrease of T(N) upon compression correlates with the anomalies in pressure behavior of Cu-O bond length and Cu-O-Cu bond angles. The reasons for the observed spin-freezing transition are discussed within the framework of the available theoretical models and the recent observation of the field-induced spin freezing.

摘要

通过中子粉末衍射和在很宽的温度和压力范围内的磁化率测量研究了氘代羟铁矾的结构和磁性。实验数据表明,在 P=2.5  GPa 时,从量子无序自旋液体相到奈尔温度 T(N)=6  K 的长程有序反铁磁相发生了转变。在压缩过程中观察到的 T(N)的降低与 Cu-O 键长和 Cu-O-Cu 键角的压力行为异常相关。在现有的理论模型的框架内以及最近观察到的磁场诱导自旋冻结的情况下,讨论了观察到的自旋冻结转变的原因。

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