论文标题
中心对称Skyrmion材料GD2PDSI3的磁相互作用
Magnetic Interactions of the Centrosymmetric Skyrmion Material Gd2PdSi3
论文作者
论文摘要
中心对称材料中磁性天际的实验实现是由对各向异性和挫败感如何稳定应用磁场中拓扑旋转结构的微妙平衡的理论理解所驱动的。最近,显示中心对称材料gd $ _ {2} $ pdsi $ _ {3} $可以主持野外诱导的Skyyrmion阶段,但Skyrmion稳定机制尚不清楚。在这里,我们在同位素增强的polycrystalline gd $ _ {2} $ pdsi $ _ {3} $样本上采用中子散射测量,以量化驱动Skyrmion组的交互。我们的分析揭示了与Rkky机制一致的三角平面中的空间扩展相互作用,并且由PD/SI上层结构调节的大型铁磁相互作用。天空阶段是从零场螺旋磁序出现的,其磁矩垂直于磁性传播载体,表明磁性偶极相互作用起着重要作用。我们的实验结果建立了一个相互作用的空间,可以促进天空形成,从而促进中心对称天际材料的鉴定和设计。
The experimental realization of magnetic skyrmions in centrosymmetric materials has been driven by theoretical understanding of how a delicate balance of anisotropy and frustration can stabilize topological spin structures in applied magnetic fields. Recently, the centrosymmetric material Gd$_{2}$PdSi$_{3}$ was shown to host a field-induced skyrmion phase, but the skyrmion stabilization mechanism remains unclear. Here, we employ neutron-scattering measurements on an isotopically-enriched polycrystalline Gd$_{2}$PdSi$_{3}$ sample to quantify the interactions that drive skyrmion formation. Our analysis reveals spatially-extended interactions in triangular planes that are consistent with an RKKY mechanism, and large ferromagnetic inter-planar magnetic interactions that are modulated by the Pd/Si superstructure. The skyrmion phase emerges from a zero-field helical magnetic order with magnetic moments perpendicular to the magnetic propagation vector, indicating that the magnetic dipolar interaction plays a significant role. Our experimental results establish an interaction space that can promote skyrmion formation, facilitating identification and design of centrosymmetric skyrmion materials.