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Microscopic origins for stabilizing room-temperature ferromagnetism in ultrathin manganite layers

机译:稳定超薄锰矿层中室温铁磁性的微观起源

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摘要

La0.7Sr0.3MnO3 is a conducting ferromagnet at room temperature. Combined with thin SrTiO3 layers, the resulting heterostructures could be used as highly spin-polarized magnetic-tunnel-junction memories. However, when shrunk to dimensions below an apparent critical thickness, the structures become insulating and ferromagnetic ordering is suppressed. Interface spin and charge modulations are thought to create an interfacial dead layer, thus fundamentally limiting the use of this material in atomic-scale devices. The thickness of this dead layer, and whether it is intrinsic, is still controversial. Here we use atomic-resolution electron spectroscopy to demonstrate that the degradation of the magnetic and transport properties of La0.7Sr0.3MnO3/SrTiO3 multilayers correlates with atomic intermixing at the interfaces, and the presence of extended two-dimensional cation defects in the La0.7Sr0.3MnO3 layers (in contrast to three-dimensional precipitates in thick films). When these extrinsic defects are eliminated, metallic ferromagnetism at room temperature can be stabilized in five-unit-cell-thick manganite layers in superlattices, placing the upper limit for any intrinsic dead layer at two unit cells per interface.
机译:La0.7Sr0.3MnO3在室温下为导电铁磁体。结合薄的SrTiO3层,所得的异质结构可以用作高度自旋极化的磁隧道结存储器。但是,当尺寸缩小到表观临界厚度以下时,结构变得绝缘,铁磁有序性受到抑制。人们认为界面自旋和电荷调制会产生界面死层,因此从根本上限制了这种材料在原子级设备中的使用。该死层的厚度以及是否为固有层仍存在争议。在这里,我们使用原子分辨率电子光谱法来证明La0.7Sr0.3MnO3 / SrTiO3多层膜的磁性和输运性能的下降与界面处的原子混合以及La0中存在扩展的二维阳离子缺陷有关。 7Sr0.3MnO3层(与厚膜中的三维沉淀相反)。当消除这些外部缺陷后,室温下的金属铁磁性可以稳定在超晶格中五单元晶格厚的锰矿层中,从而将每个界面两个单元晶格的固有固有层的上限设定为上限。

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