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Testing the Jacob's ladder of density functional for electronic structure and magnetism of rutile VO_2

机译:测试金红石VO_2的电子结构和磁性的密度泛函雅各布阶梯

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We employ semilocal density functionals [local spin-density approximation (LSDA), Perdew-Burke-Ernzerhof (PBE) generalized gradient approximation (GGA), and meta-GGAs)], LSDA plus Hubbard U (LSDA+U) theory, a nonlocal range-separated Heyd-Scuseria-Ernzerhof hybrid functional (HSE06), and the random-phase approximation (RPA) to assess their performances for the ground-state magnetism and electronic structure of a strongly correlated metal, rutile VO_2. Using recent quantum Monte Carlo results as the benchmark, all tested semilocal and hybrid functionals as well as the RPA (with PBE inputs) predict the correct magnetic ground states for rutile VO_2. The observed paramagnetism could arise from temperature-disordered local spin moments or from the thermal destruction of these moments. All semilocal functionals also give the correct ground-state metallicity for rutile VO_2. However, in the ferromagnetic (FM) and antiferromagnetic (AFM) phases, LSDA+U and HSE06 incorrectly predict rutile VO_2 to be a Mott-Hubbard insulator. For the computed electronic structures of FM and AFM phases, we find that the Tao-Perdew-Staroverov-Scuseria (TPSS) and revised TPSS (revTPSS) meta-GGAs give strong 2p-3d hybridizations, resulting in a depopulation of the 2p bands of O atoms, in comparison with other tested meta-GGAs. The regularized TPSS (regTPSS) and meta-GGAs made simple, i.e., MGGA_MS0 and MGGA_MS2, which are free of the spurious order-of-limits problem of TPSS and revTPSS, give electronic states close to those of the PBE GGA and LSDA. In comparison to experiment, semilocal functionals predict better equilibrium cell volumes for rutile VO_2 in FM and AFM states than in the spin-unpolarized state. For meta-GGAs, a monotonic decrease of the exchange enhancement factor F_x(s,α) with α for small s, as in the MGGA_MS functionals, leads to large (probably too large) local magnetic moments in spin-polarized states.
机译:我们采用半局部密度泛函[局部自旋密度近似(LSDA),Perdew-Burke-Ernzerhof(PBE)广义梯度近似(GGA)和meta-GGA],LSDA加上Hubbard U(LSDA + U)理论(非局部)范围分离的Heyd-Scuseria-Ernzerhof混合函数(HSE06)和随机相位近似(RPA)来评估它们在强相关金红石型VO_2的基态磁性和电子结构方面的性能。使用最新的量子蒙特卡洛结果作为基准,所有测试的半局部和混合功能以及RPA(带有PBE输入)可预测金红石VO_2的正确磁基态。观察到的顺磁性可能是由于温度无序的局部自旋矩或这些矩的热破坏而引起的。所有半局部官能团还为金红石VO_2提供了正确的基态金属性。但是,在铁磁(FM)和反铁磁(AFM)相中,LSDA + U和HSE06错误地将金红石VO_2预测为Mott-Hubbard绝缘子。对于FM和AFM相的计算电子结构,我们发现Tao-Perdew-Staroverov-Scuseria(TPSS)和修订的TPSS(revTPSS)meta-GGA产生强2p-3d杂交,导致2p条带的减少与其他已测试的meta-GGA相比,O原子。正规化TPSS(regTPSS)和meta-GGA变得简单,即MGGA_MS0和MGGA_MS2,它们没有TPSS和revTPSS的虚假限制顺序问题,使电子状态接近PBE GGA和LSDA的电子状态。与实验相比,半本地功能预测金红石VO_2在FM和AFM状态下比自旋非极化状态下具有更好的平衡细胞体积。对于元GGAs,交换增强因子F_x(s,α)随s的变化,随着s的减小,如MGGA_MS功能那样,会导致自旋极化状态中的局部磁矩较大(可能太大)。

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