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Exotic phases induced by strong spin-orbit coupling in ordered double perovskites

机译:有序双钙钛矿中强自旋轨道耦合引起的异相

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摘要

We construct and analyze a microscopic model for insulating rocksalt ordered double perovskites, with the chemical formula A(2)BB'O(6), where the B' atom has a 4d(1) or 5d(1) electronic configuration and forms a face-centered-cubic lattice. The combination of the triply degenerate t(2g) orbital and strong spin-orbit coupling forms local quadruplets with an effective spin moment j=3/2. Moreover, due to strongly orbital-dependent exchange, the effective spins have substantial biquadratic and bicubic interactions (fourth and sixth order in the spins, respectively). This leads, at the mean-field level, to three main phases: an unusual antiferromagnet with dominant octupolar order, a ferromagnetic phase with magnetization along the [110] direction, and a nonmagnetic but quadrupolar ordered phase, which is stabilized by thermal fluctuations and intermediate temperatures. All these phases have a two-sublattice structure described by the ordering wave vector Q=2 pi(001). We consider quantum fluctuations and argue that in the regime of dominant antiferromagnetic exchange, a nonmagnetic valence-bond solid or quantum-spin-liquid state may be favored instead. Candidate quantum-spin-liquid states and their basic properties are described. We also address the effect of single-site anisotropy driven by lattice distortions. Existing and possible future experiments are discussed in light of these results.
机译:我们用化学式A(2)BB'O(6)构造和分析绝缘岩盐有序双钙钛矿的微观模型,其中B'原子具有4d(1)或5d(1)电子构型并形成面心立方晶格。三次简并的t(2g)轨道与强自旋轨道耦合的组合形成了有效自旋矩j = 3/2的局部四联体。此外,由于强烈依赖于轨道的交换,有效的自旋具有大量的二次和双三次相互作用(分别在自旋中为四阶和六阶)。在平均场水平上,这导致了三个主要阶段:具有显性八极阶的不寻常反铁磁体,沿[110]方向磁化的铁磁相以及通过热涨落和稳定作用而稳定的非磁性但四极有序相。中间温度。所有这些相位都具有由有序波矢量Q = 2 pi(001)描述的两个子格结构。我们考虑了量子涨落,并认为在占主导地位的反铁磁交换机制中,可能更倾向于使用非磁性价键固态或量子自旋液态。描述了候选自旋液体态及其基本性质。我们还将解决由晶格畸变驱动的单点各向异性的影响。根据这些结果讨论了现有的和可能的未来实验。

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