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Microscopic Theory of Magnetic Detwinning in Iron-Based Superconductors with Large-Spin Rare Earths

机译:具有大型旋转稀土的铁基超导体中磁性扭转的微观理论

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Detwinning of magnetic (nematic) domains in Fe-based superconductors has so far only been obtained through mechanical straining, which considerably perturbs the ground state of these materials. The recently discovered nonmechanical detwinning in EuFe 2 As 2 by ultralow magnetic fields offers an entirely different, nonperturbing way to achieve the same goal. However, this way seemed risky due to the lack of a microscopic understanding of the magnetically driven detwinning. Specifically, the following issues remained unexplained: (i)?ultralow value of the first detwinning field of approximately 0.1?T, two orders of magnitude below that of BaFe 2 As 2 , and (ii)?reversal of the preferential domain orientation at approximately 1?T and restoration of the low-field orientation above 10–15?T. In this paper, we present, using published as well as newly measured data, a full theory that quantitatively explains all the observations. The key ingredient of this theory is a biquadratic coupling between Fe and Eu spins, analogous to the Fe-Fe biquadratic coupling that drives the nematic transition in this family of materials.
机译:到目前为止,Fe基超导体中的磁性(向列)域的碎屑仅通过机械紧张获得,这显着地渗透了这些材料的地面状态。 EUFE 2的最近被发现的非机械纠正为2,以外的UltraLow磁场提供了一种完全不同,不受干扰的方式来实现相同的目标。然而,这种方式由于缺乏对磁驱动的碎屑的显微镜的显微理解,似乎有风险。具体而言,以下问题仍然是未解释的:(i)?第一个纠正栏的超低值约为0.1Ω·t,额为2的两个数量级,(ii)?大约优惠域取向的逆转1?T和恢复超过10-15℃的低场取向。在本文中,我们使用已发布的以及新测量的数据,这是一种定量解释所有观察的完整理论。该理论的关键成分是Fe和Eu Spins之间的双层耦合,类似于Fe-Fe各种类型偶联,驱动该系列材料中的向志过渡。

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