论文标题
纳米平方skyrmion晶格中的中心对称四方磁铁
Nanometric square skyrmion lattice in a centrosymmetric tetragonal magnet
论文作者
论文摘要
磁性天空是具有颗粒状特征的拓扑稳定的旋转漩涡,可能适合设计高密度信息位。尽管大多数已知的天际系统是在具有dzyaloshinskii-moriya相互作用的非中心对称系统中出现的,但具有三角形晶格的中心对称磁铁也会引起天际的形成,在这种情况下,几何效率化的晶格被认为是必不可少的。直到今天,如果在没有几何效率的晶格和反转对称性破裂的情况下也可以存在Skyrmions,那么这仍然是一个悬而未决的问题。在这里,我们在中心对称四方磁铁磁铁GDRU2SI2中发现了一个方形的晶格状态,没有谐振X射线散射和Lorentz透射式透射电子显微镜实验。观察到的天空形成的合理起源是在易于轴各向异性存在下巡回电子介导的四翼相互作用。我们的结果表明,具有高度对称性晶格的稀土金属层可能会普遍存在外来起源的纳米天空含量。
Magnetic skyrmions are topologically stable spin swirls with particle-like character and potentially suitable for the design of high-density information bits. While most known skyrmion systems arise in noncentrosymmetric systems with Dzyaloshinskii-Moriya interaction, also centrosymmetric magnets with a triangular lattice can give rise to skyrmion formation, with geometrically-frustrated lattice being considered essential in this case. Until today, it remains an open question if skyrmions can also exist in the absence of both geometrically-frustrated lattice and inversion symmetry breaking. Here, we discover a square skyrmion lattice state with 1.9 nm diameter skyrmions in the centrosymmetric tetragonal magnet GdRu2Si2 without geometrically-frustrated lattice by means of resonant X-ray scattering and Lorentz transmission electron microscopy experiments. A plausible origin of the observed skyrmion formation is four-spin interactions mediated by itinerant electrons in the presence of easy-axis anisotropy. Our results suggest that rare-earth intermetallics with highly-symmetric crystal lattices may ubiquitously host nanometric skyrmions of exotic origins.