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Evidence for a Gapped Spin-Liquid Ground State in a Kagome Heisenberg Antiferromagnet

机译:Kagome Heisenberg中一个空隙旋转液体基态的证据   反铁磁

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摘要

The kagome Heisenberg antiferromagnet is a leading candidate in the searchfor a spin system with a quantum spin-liquid ground state. The nature of itsground state remains a matter of great debate. We conducted 17-O single crystalNMR measurements of the S=1/2 kagome lattice in herbertsmithiteZnCu$_3$(OH)$_6$Cl$_2$, which is known to exhibit a spinon continuum in thespin excitation spectrum. We demonstrate that the intrinsic local spinsusceptibility $\chi_{kagome}$ deduced from the 17-O NMR frequency shiftasymptotes to zero below temperature T ~ 0.03 J, where J ~ 200 K is the Cu-Cusuper-exchange interaction. Combined with the magnetic field dependence of$\chi_{kagome}$ we observed at low temperatures, these results imply that thekagome Heisenberg antiferromagnet has a spin-liquid ground state with a finitegap.
机译:kagome Heisenberg反铁磁体是寻找具有量子自旋液体基态的自旋系统的领先候选者。它的基础状态的性质仍然是一个有争议的问题。我们对HerbertsmithiteZnCu $ _3 $((OH)$ _ 6 $ Cl $ _2 $)中的S = 1/2 kagome晶格进行了17-O单晶NMR测量,已知在自旋激发光谱中会显示出自旋连续体。我们证明,在温度T〜0.03 J以下,从17-NMR频移渐近线推导出零,从而得出内在的局部自旋感$ \ chi_ {kagome} $,其中J〜200 K是Cu-Cusuper-exchange相互作用。结合我们在低温下观察到的磁场依赖性,这些结果表明,kagome海森堡反铁磁体具有具有有限间隙的自旋液体基态。

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