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首页> 外文期刊>Bulletin of the American Physical Society >APS -APS March Meeting 2017 - Event - Interfacial Spin Dephasing and Spin Absorption in Graphene Probed by Pure Spin Current
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APS -APS March Meeting 2017 - Event - Interfacial Spin Dephasing and Spin Absorption in Graphene Probed by Pure Spin Current

机译:APS -APS 2017年3月会议-事件-用纯自旋电流探测石墨烯的界面自旋相移和自旋吸收

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In order to understand the limiting factors for achieving magnetization switching using graphene, we study the spin absorption of a Fe nanomagnet deposited on a graphene spin valve. A pure spin current is injected into the graphene channel via electrical spin injection through a Co(80nm)/SrO(1nm) tunnel barrier junction. The generated pure spin current inside the graphene spin channel is partly absorbed by a nanomagnet grown on top of the spin channel allowing a direct determination of the absorbed spin current. We perform non-local magnetoresistance (MR) and Hanle spin precession measurement as we gradually deposit Fe in-situ inside an MBE chamber. We observe a rapid decrease of the non-local MR signal for a thickness ranging from 0 {AA} to 1{AA} followed by slower decrease and a saturation of the spin signal above 1 nm of Fe.Using 2D finite element modeling of the spatial distribution of the spin accumulation in the graphene channel, we extract an absorbed spin current of 2.9 x 10$^{mathrm{6}}$~A/m$^{mathrm{2}}$. By introducing a Cu spacer between the Fe and Graphene, we are able to decrease this rapid decay and observe a clear exponential decay due to the spin absorption into the Fe island. These results provide the first demonstration of interfacial spin dephasing in Graphene.
机译:为了了解使用石墨烯实现磁化转换的限制因素,我们研究了沉积在石墨烯自旋阀上的Fe纳米磁铁的自旋吸收。通过自旋注入通过Co(80nm)/ SrO(1nm)隧道势垒结将纯自旋电流注入到石墨烯通道中。石墨烯自旋通道内部生成的纯自旋电流部分被自旋通道顶部生长的纳米磁铁吸收,从而可以直接确定吸收的自旋电流。当我们在MBE腔室内逐渐原位沉积Fe时,我们执行非局部磁阻(MR)和Hanle自旋进动测量。我们观察到非局部MR信号在0 {AA}到1 {AA}范围内的厚度迅速减小,然后在Fe的1 nm以上缓慢减小并且自旋信号饱和。使用二维有限元建模,在石墨烯通道中自旋积累的空间分布中,我们提取了2.9 x 10 $ ^ {mathrm {6}} $〜A / m $ ^ {mathrm {2}} $的吸收自旋电流。通过在Fe和石墨烯之间引入Cu间隔基,我们能够减少这种快速衰减并观察到由于自旋吸收到Fe岛中而产生的明显的指数衰减。这些结果首次证明了石墨烯中的界面自旋相移。

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