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磁宇称破缺与宇称-时间反演对称磁体

Magnetic parity violation and parity-time-reversal-symmetric magnets.

作者信息

Watanabe Hikaru, Yanase Youichi

机构信息

Research Center for Advanced Science and Technology, University of Tokyo, Meguro-ku, Tokyo 153-8904, Japan.

Department of Physics, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan.

出版信息

J Phys Condens Matter. 2024 Jun 19;36(37). doi: 10.1088/1361-648X/ad52dd.

Abstract

Parity-time-reversal symmetry (PTsymmetry), a symmetry for the combined operations of space inversion (P) and time reversal (T), is a fundamental concept of physics and characterizes the functionality of materials as well asPandTsymmetries. In particular, thePT-symmetric systems can be found in the centrosymmetric crystals undergoing the parity-violating magnetic order which we call the odd-parity magnetic multipole order. While this spontaneous order leavesPTsymmetry intact, the simultaneous violation ofPandTsymmetries gives rise to various emergent responses that are qualitatively different from those allowed by the nonmagneticP-symmetry breaking or by the ferromagnetic order. In this review, we introduce candidates hosting the intriguing spontaneous order and overview the characteristic physical responses. Various off-diagonal and/or nonreciprocal responses are identified, which are closely related to the unusual electronic structures such as hidden spin-momentum locking and asymmetric band dispersion.

摘要

宇称-时间反演对称性(PT 对称性)是空间反演(P)和时间反演(T)联合操作的一种对称性,是物理学的一个基本概念,它表征了材料的功能以及 P 和 T 对称性。特别地,PT 对称系统可以在经历宇称破缺磁序(我们称之为奇宇称磁多极序)的中心对称晶体中找到。虽然这种自发序使 PT 对称性保持不变,但 P 和 T 对称性的同时破缺会产生各种涌现响应,这些响应在性质上与非磁性 P 对称性破缺或铁磁序所允许的响应不同。在这篇综述中,我们介绍了承载这种有趣自发序的候选材料,并概述了其特征性物理响应。我们识别出了各种非对角和/或非互易响应,它们与诸如隐藏自旋-动量锁定和不对称能带色散等异常电子结构密切相关。

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