焦绿石铱磁性中电子准巡回与量子有序交织在一起

Gang Chen, Xiaoqun Wang
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摘要

我们指出,磁性的产生是由焦绿石铱酸盐中电子准巡回性和量子有序无序的相互作用引起的。与其他Mott绝缘铱酸盐一样,焦绿石铱酸盐中的Ir$^{4+}$离子通过现场自旋-轨道耦合产生了有效的${J=1/2}$矩。我们考虑了焦绿石晶格上这些局部矩之间的一般对称允许交换,并得到了平均场相图。假设超交换是由中间氧直接和/或间接的电子跳跃介导的,我们从Hubbard模型中推导出强耦合状态下的交换相互作用。这种交换具有简并的经典基态流形,量子涨落选择非共面基态,称为量子有序失序。扩展到中间耦合区,通过动能从简并流形中选择出相同的非共面序,称为“电子准流动”。我们讨论了我们的结果的实验相关性和电子在其他铱酸盐和$4d/ $ 5d$磁体之间的准流动。
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Electron quasi-itinerancy intertwined with quantum order by disorder in pyrochlore iridate magnetism
We point out the emergence of magnetism from the interplay of electron quasi-itinerancy and quantum order by disorder in pyrochlore iridates. Like other Mott insulating iridates, the Ir$^{4+}$ ion in pyrochlore iridates develops an effective ${J=1/2}$ moment from the on-site spin-orbit coupling. We consider the generic symmetry-allowed exchange between these local moments on a pyrochlore lattice and obtain the mean-field phase diagram. Assuming the superexchange is mediated by direct and/or indirect electron hopping via intermediate oxygens, we derive the exchange interactions in the strong coupling regime from the Hubbard model. This exchange has a degenerate classical ground state manifold and quantum fluctuation selects a non-coplanar ground state, known as quantum order by disorder. Extending to the intermediate coupling regime, the same non-coplanar order is selected from the degenerate manifold by the kinetic energy, which is dubbed "electron quasi-itinerancy". We discuss the experimental relevance of our results and electron quasi-itinerancy among other iridates and $4d/5d$ magnets.
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