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首页> 外文期刊>Journal of Materials Research >Multivariable Study On Homoepitaxial Diamond Growth Using Isotopically Enriched Carbon-13 Gas Mixtures
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Multivariable Study On Homoepitaxial Diamond Growth Using Isotopically Enriched Carbon-13 Gas Mixtures

机译:利用同位素富集的碳13气体混合物进行同质外延金刚石生长的多变量研究

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摘要

We report our observations on the homoepitaxial diamond growth by microwave plasma chemical vapor deposition (MPCVD) experiments on Type Ib diamond substrates conducted by varying three independent variables. In a feed gas mixture of H_2, N_2, O_2, and ~(13)CH_4, the amount of nitrogen was varied in the range of 0 to 4000 ppm, the amount of methane was varied from 2% CH_4/H_2 to 6% CH_4/H_2, and the substrate temperature was varied in the range of 850 to 1200 ℃. We used isotopically enriched carbon-13 methane gas as the source of carbon in the plasma to clearly distinguish the grown diamond layer from the underlying substrate using Raman spectroscopy. The x-ray rocking curve measurements confirmed the homoepitaxial nature of the deposited layers with a slight increase in the full width at half-maximum for sample grown with the highest nitrogen content in the plasma. Optical and atomic force microscopy revealed dramatic changes in surface morphology with variation in each parameter. The nitrogen incorporation in carbon-13 diamond layers was monitored through photoluminescence spectroscopy of nitrogen-vacancy complexes. A twentyfold increase in diamond growth rate was clearly achieved in this multivariable study.
机译:我们通过改变三个独立变量对Ib型金刚石基底进行微波等离子体化学气相沉积(MPCVD)实验,报告了同质外延金刚石生长的观察结果。在H_2,N_2,O_2和〜(13)CH_4的原料气混合物中,氮的量在0至4000 ppm的范围内变化,甲烷的量在2%CH_4 / H_2至6%CH_4范围内变化/ H_2,且基板温度在850至1200℃的范围内变化。我们使用同位素富集的碳13甲烷气体作为等离子体中的碳源,以使用拉曼光谱法将生长的金刚石层与下层基底清晰地区分开。 X射线摇摆曲线测量结果证实了沉积层的同质外延特性,即对于血浆中氮含量最高的样品,其半峰全宽略有增加。光学和原子力显微镜显示表面形貌随每个参数的变化而发生巨大变化。通过氮空位络合物的光致发光光谱法监测碳13金刚石层中的氮掺入。在这项多变量研究中,钻石生长速度明显提高了20倍。

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