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arXiv 2209.00664cond-mat.str-elcond-mat.mes-hallcond-mat.mtrl-sci
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中等温度下三角晶格 Hubbard 模型的物理性质

Triangular lattice Hubbard model physics at intermediate temperatures

Kyungmin Lee, Prakash Sharma, Oskar Vafek, Hitesh J. Changlani

AI总结:

本文结合有限温 Lanczos 与 DMRG 计算,研究三角晶格 Hubbard 模型在 t≲T<U 区间的磁性,重现 WSe₂/WS₂ 莫尔双层实验中居里-外斯温度随填充的变化及反铁磁到铁磁的渡越。

摘要:

Moiré(莫尔)系统为研究强关联电子在传统材料环境中不易触及的区域内的多体效应提供了一个令人振奋的平台。受近期关于 WSe₂/WS₂ 莫尔双层体系实验的启发[Y. Tang 等人,Nature 579, 353-358 (2020)],该实验实现了一个具有小跃迁(约 10 K)和可调空穴密度的三角超晶格,我们在中等温度 t ≲ T < U 范围内研究了三角晶格上的 Hubbard 模型。采用有限温 Lanczos 计算,并严格遵循该实验所用的拟合方案,我们在采用所报道的相互作用强度 U/t=20 时,重现了所报道的居里-外斯温度 Θ 随填充变化的观测趋势。我们重点关注密度降至半填充以下时 |Θ| 的大幅增加,以及在更高填充下 Θ 的符号变化——后者标志着铁磁性的开始。在中等温度范围内,t-J 模型(Hubbard 模型的低能极限)中也可观察到 |Θ| 的增加;我们阐明这与其高温极限下的趋势相反。文中讨论了低温、中等温度和高温区域之间的差异。我们的数值计算还捕捉到了中等温度区域内从短程反铁磁序到铁磁序的渡越,这一结果与实验发现大体一致。我们发现,该行为是底层零温相变在有限温度下的残余,并通过基态密度矩阵重整化群计算对其进行了探究。我们给出了以微弱但稳健的关联为特征的铁磁性证据,这些关联解释了实验中观察到的较小 Θ。

英文摘要:

Moire systems offer an exciting playground to study many-body effects of strongly correlated electrons in regimes that are not easily accessible in conventional material settings. Motivated by a recent experiment on $\text{WSe}_2/\text{WS}_2$ moire bilayers [Y. Tang et al., Nature 579, 353-358 (2020)], which realizes a triangular superlattice with a small hopping (of approximately 10 Kelvin), with tunable density of holes, we explore the Hubbard model on the triangular lattice for intermediate temperatures $t \lesssim T < U$. Employing finite temperature Lanczos calculations, and closely following the fitting protocols used in the experiment, we recover the observed trends in the reported Curie-Weiss temperature $Θ$ with filling, using the reported interaction strength $U/t=20$. We focus on the large increase of $|Θ|$ on decreasing the density below half filling and the sign change of $Θ$ at higher fillings, which signals the onset of ferromagnetism. The increase in $|Θ|$ is also seen in the $t$-$J$ model (the low energy limit of the Hubbard model) in the intermediate temperature range, which we clarify is opposite to the trend in its high temperature limit. Differences between the low, intermediate and high temperature regimes are discussed. Our numerical calculations also capture the crossover between short-range antiferromagnetic to ferromagnetic order in the intermediate temperature regime, a result broadly consistent with the experimental findings. We find that this behavior is a finite-temperature remnant of the underlying zero temperature phase transition, which we explore with ground state density matrix renormalization group calculations. We provide evidence of ferromagnetism characterized by weak (but robust) correlations that explain the small $Θ$ seen in the experiment.

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