FMR测量证明了钠掺杂锰的超薄膜的面外自旋排列

A. Tovstolytkin, A. Pogorily, V. V. Dzyublyuk, D.I. Podylalovskii, A. Matviyenko
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引用次数: 0

摘要

稀土离子R和碱性(或碱土)离子A掺杂的钙钛矿锰矿RAMnO3因其有趣的磁性、磁阻性和微波性能而受到广泛关注[1,2,3]。很多的努力,无论是理论还是实验,都致力于研究与它们非凡的磁阻行为相关的潜在物理学。相比之下,对磁各向异性和微磁结构等磁性能的研究非常有限,而相关知识显然是设计和制造自旋阀、隧道结等异质外延器件的先决条件[4]。
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Out-of-plane spin alighnment in ultrathin films of sodium-doped manganites as evidenced by FMR measurements
Doped perovskite manganites RAMnO3 with rare-earth ions R and alkaline (or alkaline-earth) ions A have received considerable attention because of their interesting magnetic, magnetoresistive, and microwave properties [1,2,3]. Much effort, both theoretical and experimental, has been devoted to the investigation of the underlying physics associated with their extraordinary magnetoresistive behavior. In contrast, work on magnetic properties such as magnetic anisotropy and micromagnetic structure is very limited, while the relevant knowledge is obviously a prerequisite for the design and fabrication of heteroepitaxy devices such as spin valves, tunneling junctions, and etc. [4].
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