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CN distribution in flame deposition of diamond and its relation to the growth rate, morphology, and nitrogen incorporation of the diamond layer

机译:金刚石火焰沉积中的CN分布及其与金刚石层的生长速率,形态和氮结合的关系

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摘要

Two-dimensional laser-induced fluorescence (2D-LIF) measurements are applied to the chemicalvapour deposition (CVD) of diamond by an oxyacetylene flame to visualize the distribution of CN inthe gas phase during the diamond growth process. The obtained diamond deposits are characterizedby optical as well as scanning electron microscopy (SEM) and cathodoluminescence topography(CL). Experiments are carried out in both laminar and turbulent flames and show CN to be presentmostly at the outer edge of the flame, where ambient air interacts with flame gases. Clear relationsare observed between the distribution of CN and the local variation of the growth rate, themorphology, and the nitrogen incorporation as identified by CL in the deposited diamond layer. Theobserved differences between the laminar and turbulent flame can be attributed to enhanced diffusionof nitrogen into the latter. Significant differences are found between the results of experimentsperformed with acetylene gas bottles from two different suppliers.
机译:通过氧乙炔火焰将二维激光诱导的荧光(2D-LIF)测量应用于金刚石的化学气相沉积(CVD),以可视化金刚石生长过程中气相中CN的分布。所得的金刚石沉积物通过光学以及扫描电子显微镜(SEM)和阴极发光形貌(CL)表征。在层流和湍流火焰中都进行了实验,结果表明CN最主要位于火焰的外边缘,在该边缘,环境空气与火焰气体相互作用。在沉积的金刚石层中,CN的分布与生长速率,形貌和氮掺入的局部变化之间观察到明确的关系。层流火焰和湍流火焰之间观察到的差异可归因于氮向后者的扩散增强。发现使用两个不同供应商的乙炔气瓶进行的实验结果之间存在显着差异。

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