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首页> 外文期刊>Bulletin of the American Physical Society >APS -APS March Meeting 2017 - Event - George E. Valley, Jr. Prize Talk: Quantum Frustrated Magnetism and its Expression in the Ground State Selection of Pyrochlore Magnets
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APS -APS March Meeting 2017 - Event - George E. Valley, Jr. Prize Talk: Quantum Frustrated Magnetism and its Expression in the Ground State Selection of Pyrochlore Magnets

机译:APS -APS 2017年3月会议-活动-乔治·E·瓦利,小奖演讲:量子受挫磁性及其在烧绿石磁体基态选择中的表达

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摘要

In the search for novel quantum states of matter, such as highly entangled Quantum Spin Liquids, ``geometrically frustrated'' magnetic lattices are essential for suppressing conventional magnetic order. In three dimensions, the pyrochlore lattice is the canonical frustrated geometry. Magnetic materials with pyrochlore structures have the potential to realize unusual phases such as ``quantum spin ice'', which is predicted to host emergent magnetic monopoles, electrons, and photons as its fundamental excitations. Even in pyrochlores that form long range ordered phases, this often occurs through unusual routes such as ``order by disorder'', in which the fluctuation spectrum dictates the preferred ordered state. The rare earth-based pyrochlore series $R_2$Ti$_2$O$_7$ provides a fascinating variety of magnetic ground states. I will introduce the general anisotropic interaction Hamiltonian that has been successfully used to describe several materials in this series. Using inelastic neutron scattering, the relevant anisotropic interaction strengths can be extracted quantitatively. I will discuss this approach, and its application to two rare earth pyrochlore materials, Er$_2$Ti$_2$O$_7$ and Yb$_2$Ti$_2$O$_7$, whose ground state properties have long been enigmatic. From these studies, Er$_2$Ti$_2$O$_7$ and Yb$_2$Ti$_2$O$_7$ have been suggested to be realizations of ``quantum order by disorder'' and ``quantum spin ice'', respectively.
机译:在寻找新的物质量子态(例如高度纠缠的量子自旋液体)时,``几何受挫''的磁晶格对于抑制常规磁阶至关重要。在三个维度上,烧绿石晶格是规范的受挫几何形状。具有烧绿石结构的磁性材料具有实现不寻常相的潜力,例如``量子自旋冰'',据预测,该相将以新兴的磁性单极子,电子和光子为基本激发源。即使在形成远距离有序相的烧绿石中,这也经常通过不寻常的途径发生,例如``无序排序'',其中波动谱决定了优选的有序状态。稀土基烧绿石系列$ R_2 $ Ti $ _2 $ O $ _7 $提供了引人入胜的各种磁性基态。我将介绍已成功用于描述本系列中几种材料的一般各向异性相互作用哈密顿量。使用非弹性中子散射,可以定量地提取相关的各向异性相互作用强度。我将讨论这种方法及其在两种稀土烧绿石材料中的应用,即Er $ _2 $ Ti $ _2 $ O $ _7 $和Yb $ _2 $ Ti $ _2 $ O $ _7 $,它们的基态特性长期以来一直是令人迷惑的。从这些研究中,Er $ _2 $ Ti $ _2 $ O $ _7 $和Yb $ _2 $ Ti $ _2 $ O $ _7 $被认为是``无序量子序''和``量子自旋冰''的实现。 '', 分别。

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