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Self-organized homo-epitaxial growth of (001) vanadium assisted by oxygen surface reconstruction

机译:氧表面重构辅助(001)钒的自组织均质外延生长

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In this paper the effect of oxygen on the vanadium homoepitaxial growth process is analyzed by using Auger spectroscopy, electron diffraction and scanning tunneling microscopy. As the oxygen induced 1 x 5 surface structure got a lattice spacing 6% different from the pure V lattice, relaxation is observed by electron diffraction during the growth. The average in-plane lattice spacing is thus shown to be proportional to the oxygen surface concentration. The surface lattice relaxation is observed to exponentially vary with the number of deposited atomic planes. A kinetic model is proposed and allows us to explain these observations. Furthermore, it helps us to distinguish two regimes depending on growth temperature. At high temperature, the oxygen surface concentration during growth is due to oxygen upward diffusion from the underneath V layer. For lower temperature however, this upward diffusion is not efficient and another source of oxygen contamination is evidenced. When the oxygen surface concentration is sufficient, a spectacular self-organization is observed at the surface by surface microscopy. Ribbons shape islands are observed and are tentatively explained as a consequence of oxygen surface concentration and stress induced by the surface reconstruction. (C) 2016 Elsevier B.V. All rights reserved.
机译:本文利用俄歇光谱,电子衍射和扫描隧道显微镜分析了氧对钒同质外延生长过程的影响。由于氧诱导的1 x 5表面结构的晶格间距与纯V晶格不同,因此在生长过程中通过电子衍射观察到弛豫。因此,平均面内晶格间距与氧气表面浓度成正比。观察到表面晶格弛豫随沉积的原子平面的数量呈指数变化。提出了动力学模型,并允许我们解释这些观察结果。此外,它有助于我们根据生长温度来区分两种情况。在高温下,生长过程中的氧气表面浓度是由于氧气从下方的V层向上扩散所致。然而,对于较低的温度,这种向上扩散是无效的,并且证明了另一种氧污染源。当氧气表面浓度足够时,通过表面显微镜在表面观察到壮观的自组织。由于氧表面浓度和表面重建引起的应力,因此观察到并初步解释了带状岛。 (C)2016 Elsevier B.V.保留所有权利。

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