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Ferroic nature of magnetic toroidal order

机译:磁环序的铁性

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Electric dipoles and ferroelectricity violate spatial inversion symmetry, and magnetic dipoles and ferromagnetism break time-inversion symmetry. Breaking both symmetries favours magnetoelectric charge-spin coupling effects of enormous interest, such as multiferroics, skyrmions, polar superconductors, topological insulators or dynamic phenomena such as electromagnons. Extending the rationale, a novel type of ferroic order violating space- and time-inversion symmetry with a single order parameter should exist. This existence is fundamental and the inherent magnetoelectric coupling is technologically interesting. A uniform alignment of magnetic vortices, called ferrotoroidicity, was proposed to represent this state. Here we demonstrate that the magnetic vortex pattern identified in LiCoPO4 exhibits the indispensable hallmark of such a ferroic state, namely hysteretic poling of ferrotoroidic domains in the conjugate toroidal field, along with a distinction of toroidal from non-toroidal poling effects. This consolidates ferrotoroidicity as fourth form of ferroic order.
机译:电偶极子和铁电违反了空间反演对称性,而磁偶极子和铁磁性打破了时间反演对称性。打破这两个对称性有利于引起人们极大兴趣的磁电电荷自旋耦合效应,例如多铁磁,天空粒子,极性超导体,拓扑绝缘体或动态现象,例如电磁子。扩展理论基础,应该存在一种新颖的,具有单阶参数的,违反空间和时间反演对称性的铁阶。这种存在是基础,固有的磁电耦合在技术上很有趣。提出了称为铁磁环性的磁涡旋的均匀排列来表示这种状态。在这里,我们证明了在LiCoPO4中识别出的磁涡旋图表现出这种铁磁状态的必不可少的标志,即在共轭环形场中铁磁环形域的磁滞极化,以及从非环形极化效应中区分出了环形。这将铁磁环性巩固为铁磁有序的第四种形式。

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