氧乙炔生长金刚石火焰中H、CN、C2的空间分布

R.J.H. Klein-Douwel, J.J. Ter Meulen
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引用次数: 0

摘要

二维激光诱导荧光(2D-LIF)测量应用于化学气相沉积(CVD)金刚石氧乙炔火焰可视化原子氢,C2和CN在金刚石生长过程中的气相分布。在层流火焰中进行了实验,发现原子氢在火焰前缘及火焰前缘以外普遍存在。它的存在延伸到金刚石沉积区之外,而C2的分布仅限于火焰前缘和乙炔羽。发现CN主要存在于火焰的外缘,在那里环境空气与火焰气体相互作用。利用光学、扫描电镜(SEM)和阴极发光形貌(CL)对所得金刚石层进行了表征。观察到金刚石层生长速率的局部变化与衬底上方边界层中H、C2和CN的分布之间存在明显的关系。此外,还发现了CN与沉积金刚石层的形态和含氮量之间的进一步关系。这些关系与描述上述物质在金刚石(火焰)沉积过程中重要性的理论模型一致。在火焰层和金刚石层中可以分辨出三个独立的区域,其中气相和金刚石的生长主要分别受火焰源气体、周围大气以及两者的相互作用的支配。
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Spatial distributions of H, CN, and C2 in a diamond-growing oxyacetylene flame

Two-dimensional laser-induced fluorescence (2D-LIF) measurements are applied to the chemical vapor deposition (CVD) of diamond by an oxyacetylene flame to visualize the distributions of atomic hydrogen, C2, and CN in the gas phase during diamond growth. Experiments are carried out in laminar flames and reveal that atomic hydrogen is ubiquitous at and beyond the flame front. Its presence extends to well outside the diamond deposition region, whereas the C2 distribution is limited to the flame front and the acetylene feather. CN is found to be present mostly at the outer edge of the flame, where ambient air interacts with flame gases. The diamond layers obtained are characterized by optical as well as scanning electron microscopy (SEM) and cathodoluminescence topography (CL). Clear relations are observed between the local variations in growth rate of the diamond layer and the distribution of H, C2, and CN in the boundary layer just above the substrate. Further relations between CN and the morphology and the nitrogen incorporation as identified by CL of the deposited diamond layer are found as well. These relations agree with theoretical models describing the importance of the mentioned species in (flame) deposition processes of diamond. Three separate regions can be discerned in the flame and the diamond layer, where the gas phase and diamond growth are predominantly governed by the flame source gases, the ambient atmosphere, and the interaction of both, respectively.

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