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首页> 外文期刊>Journal of Applied Physics >Interface magnetism and magnetic structure of GdN/Fe multilayers studied by x-ray magnetic circular dichroism
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Interface magnetism and magnetic structure of GdN/Fe multilayers studied by x-ray magnetic circular dichroism

机译:X射线磁性圆二色性研究GdN / Fe多层膜的界面磁性和磁性结构

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摘要

We have used the element specificity of x-ray magnetic circular dichroism to separate the contributions of the component layers to the magnetization and local magnetic structure of artificial nanoscale ferrimagnetic multilayers GdN/Fe. The Fe layers, by strong antiferromagnetic interlayer exchange coupling, not only magnetize a narrow interface region in paramagnetic GdN but induce long-range magnetic order in the volume of the GdN layers at temperatures considerably above the Curie temperature of the bare layers (T_C~(GdN) ≈ 60 K), in support of a theoretical mean-field prediction. We propose that the effect may be related to the special electronic band structure of GdN, which shows a transition from narrow-gap semiconducting to metallic conduction at T_C~(GdN). In an elevated external magnetic field the GdN- and Fe-sublayer magnetic moments adopt a canted configuration. In this state the local magnetization in each GdN layer is highly nonuniform at low temperature. The interior turns its moment into the field direction almost abruptly from one atomic layer to the next in a single block. This indicates weak magnetic coupling between the interfacial and volume magnetizations in GdN. The results are at variance with the much studied "model" multilayer system Gd/Fe, where magnetic order in the Gd-layer volume appears intrinsically only significantly below the Curie temperature of bulk Gd. Furthermore, magnetization reversal in the Gd layers in a magnetic field occurs gradually on a considerably larger length scale, only if they are sufficiently thick.
机译:我们已经使用X射线磁性圆二色性的元素特异性来分离组分层对人工纳米级亚铁磁性多层GdN / Fe的磁化和局部磁结构的贡献。通过强反铁磁性层间交换耦合,Fe层不仅在顺磁性GdN中磁化了狭窄的界面区域,而且在明显高于裸层居里温度(T_C〜( GdN)≈60 K),以支持理论上的平均场预测。我们认为该效应可能与GdN的特殊电子能带结构有关,该结构显示了在T_C〜(GdN)处从窄隙半导体向金属导电的过渡。在升高的外部磁场中,GdN和Fe子层磁矩采用倾斜构造。在这种状态下,每个GdN层中的局部磁化强度在低温下非常不均匀。内部几乎在一个块中突然从一个原子层到下一个原子层将其力矩转换为场方向。这表明GdN中界面磁化和体积磁化之间的弱磁耦合。结果与经过大量研究的“模型”多层系统Gd / Fe不一致,在该系统中,Gd层体积中的磁序本质上仅显着低于块状Gd的居里温度。此外,只有当它们足够厚时,磁场中的Gd层中的磁化反转才会以相当大的长度尺度逐渐发生。

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