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室温下在平面α-FeO/Co异质结构中对磁涡旋对的观测。

Observation of magnetic vortex pairs at room temperature in a planar α-FeO/Co heterostructure.

作者信息

Chmiel F P, Waterfield Price N, Johnson R D, Lamirand A D, Schad J, van der Laan G, Harris D T, Irwin J, Rzchowski M S, Eom C-B, Radaelli P G

机构信息

Clarendon Laboratory, Department of Physics, University of Oxford, Oxford, UK.

Diamond Light Source, Harwell Science and Innovation Campus, Didcot, UK.

出版信息

Nat Mater. 2018 Jul;17(7):581-585. doi: 10.1038/s41563-018-0101-x. Epub 2018 Jun 18.

DOI:10.1038/s41563-018-0101-x
PMID:29915425
Abstract

Vortices, occurring whenever a flow field 'whirls' around a one-dimensional core, are among the simplest topological structures, ubiquitous to many branches of physics. In the crystalline state, vortex formation is rare, since it is generally hampered by long-range interactions: in ferroic materials (ferromagnetic and ferroelectric), vortices are observed only when the effects of the dipole-dipole interaction are modified by confinement at the nanoscale, or when the parameter associated with the vorticity does not couple directly with strain . Here, we observe an unprecedented form of vortices in antiferromagnetic haematite (α-FeO) epitaxial films, in which the primary whirling parameter is the staggered magnetization. Remarkably, ferromagnetic topological objects with the same vorticity and winding number as the α-FeO vortices are imprinted onto an ultra-thin Co ferromagnetic over-layer by interfacial exchange. Our data suggest that the ferromagnetic vortices may be merons (half-skyrmions, carrying an out-of plane core magnetization), and indicate that the vortex/meron pairs can be manipulated by the application of an in-plane magnetic field, giving rise to large-scale vortex-antivortex annihilation.

摘要

涡旋是最简单的拓扑结构之一,只要流场围绕一维核心“旋转”就会出现,在许多物理分支中都很常见。在晶体状态下,涡旋形成很少见,因为它通常受到长程相互作用的阻碍:在铁电材料(铁磁和铁电)中,只有当偶极-偶极相互作用的影响通过纳米尺度的限制得到改变,或者与涡度相关的参数不直接与应变耦合时,才会观察到涡旋。在这里,我们在反铁磁赤铁矿(α-FeO)外延薄膜中观察到一种前所未有的涡旋形式,其中主要的旋转参数是交错磁化强度。值得注意的是,具有与α-FeO涡旋相同涡度和缠绕数的铁磁拓扑对象通过界面交换被印刻在超薄Co铁磁覆盖层上。我们的数据表明,铁磁涡旋可能是磁子(半斯格明子,携带面外核心磁化强度),并表明涡旋/磁子对可以通过施加面内磁场来操纵,从而导致大规模的涡旋-反涡旋湮灭。

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