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首页> 外文期刊>Physical Review, B. Condensed Matter >Magnetic structure of Fe/Gd multilayers determined by resonant x-ray magnetic scattering
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Magnetic structure of Fe/Gd multilayers determined by resonant x-ray magnetic scattering

机译:通过共振X射线磁散射确定Fe / Gd多层膜的磁性结构

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The magnetic structures of a (Fe/Gd)(15) multilayer are determined by resonant x-ray magnetic scattering using circular polarized light of energies tuned close to the Gd L and the Fe K absorption edges. Difference superlattice Bragg peaks observed by flipping the photon helicity show that the magnetic moments of the Gd layers are directed antiparallel to the in-plane applied held at temperatures higher than 180 K, and are twisted below. The local Gd magnetizations in each 5.4-nm-thick layer are highly nonuniform in both magnitude and twist angle in the out-of-plane direction: the interface sublayers nearly fully magnetize at room and low temperatures under the influence of the adjacent Fe magnetizations, whereas the central sublayers show measurable spontaneous magnetizations at 200 K and below. An application of the 1 -(T/T-c) law shows a reduced Curie temperature (T-c=214 K) compared with bulk Gd for the central sublayers, while T-c= 1023 K for the interface sublayers. The interface and central sublayers exhibit distinct twist behaviors as a function of temperature below the compensation temperature, indicating the short-range nature of the Fe-Gd interaction. The element-specific resonant x-ray scattering confirmed the antiferromagnetic arrangement of the Gd and Fe moments at room temperature. [References: 29]
机译:(Fe / Gd)(15)多层膜的磁性结构是通过共振X射线磁散射确定的,其中使用的圆形偏振光的能量被调整为接近Gd L和Fe K吸收边缘。通过翻转光子螺旋度观察到的不同超晶格布拉格峰表明,Gd层的磁矩与保持在高于180 K的温度下所施加的面内反平行地定向,并且在下方扭曲。每个5.4 nm厚层中的局部Gd磁化强度在面外方向上的大小和扭曲角度均非常不均匀:在相邻的Fe磁化强度的影响下,界面子层在室温和低温下几乎完全磁化,而中心子层在200 K及以下时显示出可测量的自发磁化强度。 1-(T / T-c)法则的应用显示,与中央子层的体Gd相比,居里温度降低了(T-c = 214 K),而界面子层的T-c = 1023K。界面和中间子层表现出明显的扭曲行为,这些扭曲行为是低于补偿温度的温度的函数,表明Fe-Gd相互作用的短距离性质。特定于元素的共振X射线散射证实了室温下Gd和Fe矩的反铁磁排列。 [参考:29]

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