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Static and dynamical spin correlations of the S=1/2 random-bond antiferromagnetic Heisenberg model on the triangular and kagome lattices

机译:S = 1/2随机键反铁磁Heisenberg模型在三角形和Kagome晶格上的静态和动态自旋相关性

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摘要

Inspired by the recent theoretical suggestion that the random-bond 5=1/2 antiferromagnetic Heisenberg model on the triangular and the kagome lattices might exhibit a randomness-induced quantum spin liquid (QSL) behavior when the strength of the randomness exceeds a critical value, and that this "random-singlet state" might be relevant to the QSL behaviors experimentally observed in triangular organic salts κ-(ET)_2Cu_2(CN)_3 and EtMe_3Sb[Pd(dmit)_2]_2 and in kagome herbertsmithite ZnCu_3(OH)_6Cl_2, we further investigate the nature of the static and the dynamical spin correlations of these models. We compute the static and the dynamical spin structure factors, S(q) and 5(q,ω), by means of an exact diagonalization method. In both triangular and kagome models, the computed 5(q,ω) in the random-singlet state depends on the wave vector q only weakly, robustly exhibiting gapless behaviors accompanied by the broad distribution extending to higher energy ω. Especially in the strongly random kagome model, 5(q,ω) hardly depends on q, and exhibits an almost flat distribution for a wide range of ω, together with a ω= 0 peak. These features agree semiquantitatively with the recent neutron-scattering data on a single-crystal herbertsmithite. Furthermore, the computed magnetization curve agrees almost quantitatively with the experimental one recently measured on a single-crystal herbertsmithite. These results suggest that the QSL state observed in herbertsmithite might indeed be the randomness-induced QSL state, i.e., the random-singlet state.
机译:受最新理论建议的启发,当随机强度超过临界值时,三角形和kagome晶格上的随机键5 = 1/2反铁磁海森堡模型可能会表现出由随机性引起的量子自旋液体(QSL)行为,并且该“随机单态”可能与在三角形有机盐κ-(ET)_2Cu_2(CN)_3和EtMe_3Sb [Pd(dmit)_2] _2和kagome钙铁矿ZnCu_3(OH)中实验观察到的QSL行为有关_6Cl_2,我们将进一步研究这些模型的静态和动态自旋相关性。我们通过精确的对角线化方法来计算静态和动态自旋结构因子S(q)和5(q,ω)。在三角模型和kagome模型中,在随机单峰状态下计算出的5(q,ω)仅微弱地依赖于波矢量q,鲁棒地表现出无间隙行为,并伴随着扩展到较高能量ω的宽分布。特别是在强随机kagome模型中,5(q,ω)几乎不依赖于q,并且在宽范围的ω上都表现出几乎平坦的分布,并且ω= 0峰。这些特征半定量地与最近在单晶铁矾石上的中子散射数据一致。此外,计算出的磁化曲线几乎与最近在单晶铁矾石上测得的实验曲线基本一致。这些结果表明,在铁长石中观察到的QSL状态确实可能是由随机性引起的QSL状态,即,随机-单重状态。

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  • 来源
    《Physical review》 |2015年第13期|134407.1-134407.12|共12页
  • 作者单位

    Department of Earth and Space Science, Graduate School of Science, Osaka University, Toyonaka, Osaka 560-0043, Japan;

    Department of Earth and Space Science, Graduate School of Science, Osaka University, Toyonaka, Osaka 560-0043, Japan;

    Department of Earth and Space Science, Graduate School of Science, Osaka University, Toyonaka, Osaka 560-0043, Japan;

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  • 正文语种 eng
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  • 关键词

    quantized spin models; spin-glass and other random models;

    机译:量化自旋模型自旋玻璃和其他随机模型;

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