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Higgs transition from a magnetic Coulomb liquid to a ferromagnet in Yb2Ti2O7

机译:希格斯在Yb2Ti2O7中从磁性库仑液体转变为铁磁体

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摘要

In a class of frustrated magnets known as spin ice, magnetic monopoles emerge as classical defects and interact via the magnetic Coulomb law. With quantum-mechanical interactions, these magnetic charges are carried by fractionalized bosonic quasi-particles, spinons, which can undergo Bose–Einstein condensation through a first-order transition via the Higgs mechanism. Here, we report evidence of a Higgs transition from a magnetic Coulomb liquid to a ferromagnet in single-crystal Yb2Ti2O7. Polarized neutron scattering experiments show that the diffuse [111]-rod scattering and pinch-point features, which develop on cooling are suddenly suppressed below TC~0.21 K, where magnetic Bragg peaks and a full depolarization of the neutron spins are observed with thermal hysteresis, indicating a first-order ferromagnetic transition. Our results are explained on the basis of a quantum spin-ice model, whose high-temperature phase is effectively described as a magnetic Coulomb liquid, whereas the ground state shows a nearly collinear ferromagnetism with gapped spin excitations.
机译:在称为自旋冰的一类沮丧的磁体中,磁性单极子作为经典缺陷出现并通过库仑磁定律相互作用。通过量子力学相互作用,这些磁性电荷被分数阶的拟声子准直子,旋子所携带,它们可以通过希格斯机制通过一阶跃迁经历玻色-爱因斯坦凝聚。在这里,我们报告了单晶Yb2Ti2O7中从磁性库仑液体到铁磁体的希格斯跃迁的证据。极化中子散射实验表明,在TC〜0.21 K以下,在冷却过程中产生的扩散[111]-棒散射和收缩点特征突然被抑制,在该温度下观察到磁布拉格峰和中子自旋完全去极化,并具有热滞现象,表示一阶铁磁跃迁。我们的结果是基于量子自旋冰模型进行解释的,该模型的高温相被有效地描述为磁性库仑液体,而基态显示出具有空缺自旋激发的近似共线铁磁性。

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