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首页> 外文期刊>Russian Microelectronics >A Study of Magnetic and Electronic Hyperfine Interactions in Epitaxial Film of Yttrium-Iron Garnet by the Method of Conversion Electron Mossbauer Spectroscopy
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A Study of Magnetic and Electronic Hyperfine Interactions in Epitaxial Film of Yttrium-Iron Garnet by the Method of Conversion Electron Mossbauer Spectroscopy

机译:转换电子豆类素光谱法的钇 - 铁石榴石外延薄膜磁性和电子高浓度的研究

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摘要

Magnetic and electric hyperfine interactions in the near-surface layers of epitaxial films of yttrium-iron garnet of the (111) orientation grown by the liquid-phase epitaxy method are studied by the method of the conversion electron Mossbauer spectroscopy (CEMS). The studies reveal a stoichiometric violation of the anion sublattice in the near-surface layers (≈8 × 10~(-8) m) of yttrium iron garnet film and, as a consequence, the formation of two types of d-sites, which is associated with a significant concentration of point defects in the anion sublattice of the near-surface area and the growing weight of the covalent bonding in the transition film-air layer. This also causes the presence of a fixed doublet component corresponding to iron ions in a paramagnetic state with an intermediate degree of valency between +2 and +3. It is shown that interpretation of the spectroscopic results using the Hamiltonian of mixed magnetic and quadrupole interactions makes it possible to obtain a vector diagram of the spatial orientations of the effective magnetic fields at the Fe~(57) nuclei and, as a consequence, to reconstruct the formation mechanism of the resulting vector of the magnetic moment of the yttrium iron garnet epitaxial film. Our studies reveal a slight noncollinearity of ≈4° in the orientations of the magnetic moments in the a- and d-sites of iron. The obtained results complement the picture of the magnetic and electronic hyperfine interactions in the epitaxial ferrite-garnet films and should be considered in the practical applications of the magnetic properties of such materials.
机译:通过转化电子豆类素光谱(CEMS)的方法研究了由液相外延方法生长的(111)取向的yttrium-Iron Garnet的近表面层中的磁性和电动血清相互作用。这些研究揭示了在近地面层(≈8×10〜(-8)米)的钇铁石榴膜中的阴离子子变量的化学计量侵犯,因此,形成两种类型的D型位点,这与近表面区域的阴离子子阴离子的显着浓度的点缺陷和过渡膜 - 空气层中的共价键合的重量的显着缺陷相关。这也使得在顺磁状态下存在与铁离子相对应的固定双重组分,其中+ 2和+3之间的中间值。结果表明,使用混合磁性和四极相互作用的汉密尔顿汉尼西亚的光谱结果解释使得可以获得Fe〜(57)核的有效磁场的空间取向的矢量图,并且因此重建钇铁石榴石外延膜磁矩的形成载体的形成机制。我们的研究揭示了铁的A-和D型位点的磁矩的方向上的略微非粘附性。所获得的结果补充了外延铁氧体 - 石榴石膜中的磁性和电子高浓度相互作用的图像,并且应该在这些材料的磁性的实际应用中考虑。

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