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In situ small-angle x-ray and nuclear resonant scattering study of the evolution of structural and magnetic properties of an Fe thin film on MgO (001)

机译:原位小角X射线和核共振散射研究MgO(001)上Fe薄膜的结构和磁性的演变

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摘要

Growth of magnetron sputtered Fe films on clean single crystalline MgO (001) substrate has been studied using in situ grazing incidence small angle x-ray scattering (GISAXS) and grazing incidence nuclear resonant scattering (GINRS) measurements. While GISAXS provides information about morphological changes, GINRS provides information about structural and magnetic properties, thus making it possible to correlate the evolution of magnetic properties with that of morphology and structure of the film. The film exhibits a Volmer-Weber type growth, with percolation transition occurring around 2 nm film thickness. Presence of a finite quadrupole splitting, as seen in GINRS measurements, suggests a significant distortion from cubic symmetry up to a film thickness of 3.5 nm, which can be attributed to hybridization between Fe 3d and O 2p orbitals at the interface as well as in-plane tensile strain induced as a result of coalescence of islands. Initially Fe islands exhibit superparamagnetic relaxation, while finite magnetic moment appears upon formation of macroscopic percolation islands. The film exhibits a weak perpendicular magnetic anisotropy (PMA), which vanishes concurrently with disappearance of structural distortion, suggesting that the observed PMA at least partly originates from inherent strain in the film. No presence of any known oxide of Fe was detected at the interface. More precise information about topological and magnetic structure of the interfaces between Fe and MgO layers is obtained using combined x-ray reflectivity and nuclear resonance reflectivity measurements on a $^{57}$Fe/MgO multilayer. Measurements show that about two monolayers of Fe at the interface have a reduced hyperfine field, providing evidence for hybridization with O atoms, as predicted by theory.
机译:使用原位掠入射小角X射线散射(GISAXS)和掠入射核共振散射(GINRS)测量研究了磁控溅射Fe膜在干净的单晶MgO(001)衬底上的生长。 GISAXS提供有关形态变化的信息,而GINRS提供有关结构和磁性能的信息,因此可以将磁性能的演变与薄膜的形态和结构联系起来。该膜表现出Volmer-Weber型生长,在2 nm左右的膜厚附近发生渗滤转变。如在GINRS测量中所见,存在有限的四极分裂,表明立方对称性直至3.5 nm的膜厚都存在明显的畸变,这可能归因于界面处的Fe 3d和O 2p轨道之间的杂化以及由于岛的融合而引起的平面拉伸应变。最初,Fe岛表现出超顺磁弛豫,而在形成宏观渗流岛时出现有限的磁矩。该膜表现出弱的垂直磁各向异性(PMA),随着结构变形的消失而消失,这表明所观察到的PMA至少部分源自膜中的固有应变。在界面处未检测到任何已知的Fe氧化物。关于Fe和MgO层之间界面的拓扑和磁性结构的更精确信息,是通过在x ^ {57} $ Fe / MgO多层膜上使用组合的x射线反射率和核共振反射率测量获得的。测量表明,界面上大约两个单层的Fe具有减小的超精细场,这为理论上的预测提供了与O原子杂交的证据。

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