掺杂硅/钴的铁锗自旋纹理的拓扑稳定性

Yao Guang, Yukako Fujishiro, Aito Tanaka, Licong Peng, Yoshio Kaneko, Naoya Kanazawa, Yoshinori Tokura, Xiuzhen Yu
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摘要

众所周知,磁性或非磁性原子的元素置换会显著影响磁体的磁性结构和相关传输特性。为了弄清掺杂元素后 B20 型磁体磁性结构的变化,我们对分别用 Co 和 Si 部分取代 Fe 和 Ge 的螺旋磁体 FeGe 的自旋纹理及其温度(T)-磁场(H)相图进行了实空间观测。螺旋周期(λ)因元素掺杂而发生显著变化:与 FeGe 中的λ = 70 nm 相比,掺杂 30% Co 的 FeGe 中的λ 增加了 147% 至 103 nm,而掺杂 30% Si 的 FeGe 中的λ 则减少了约 70% 至 49 nm。在对FeSi0.3Ge0.7和Fe0.7Co0.3Ge的(001)、(110)和(111)薄板正常施加磁场时,会出现六方天幕晶体(SkX)态。通过实空间成像观察到的磁相图显示:(1) 通过减小样品厚度或在特定磁场下从高于转变温度 (TC) 的温度开始冷却样品,SkX 可以扩展到更大的 T-H 窗口;(2) 掺 Si 和掺 Co 的 FeGe 中 SkX 相的稳定性不同:在 (111) FeSi0.3Ge0.7 中 SkX 相最不稳定,而在 (111) Fe0.7Co0.3Ge 中则保持稳定。这些差异表明,掺杂磁性元素(Co)和非磁性元素(Si)的 FeGe 具有不同的各向异性。
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Topological stability of spin textures in Si/Co-doped helimagnet FeGe
Element substitutions with magnetic or non-magnetic atoms are known to significantly impact the magnetic structure and related transport properties of magnets. To clarify the change of magnetic structure of B20-type magnets with element doping, we conduct real-space observations of spin textures and their temperature (T)-magnetic field (H) phase diagrams of a helimagnet FeGe with partially substituting Fe and Ge with Co and Si, respectively. The helical period (λ) changes dramatically by the element doping: λ increases by 147% to 103 nm in 30% Co-doped FeGe, whereas it decreases by around 70% to 49 nm in 30% Si-doped FeGe, compared to the λ =70 nm in FeGe. Upon applying the magnetic field normally to (001), (110), and (111) thin plates of both FeSi0.3Ge0.7 and Fe0.7Co0.3Ge, the hexagonal skyrmion crystal (SkX) state emerges. The magnetic phase diagrams observed through the real-space imaging reveal that (1) the SkX can extend to a larger T-H window by reducing the sample thickness or by cooling the sample under specific magnetic fields from temperatures above the transition temperature (TC ); (2) the stability of the SkX phase differs between Si-doped and Co-doped FeGe: the SkX phase is most unstable in the (111) FeSi0.3Ge0.7, while it remains robust in the (111) Fe0.7Co0.3Ge. These differences indicate distinct anisotropic behavior in FeGe with magnetic (Co) and non-magnetic-element (Si) dopants.
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