Sulfur and Sodium: Diffusion of Potential Donors into Natural Diamond

M. West, M. Prelas, R. Tompson, A. Khomich
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引用次数: 1

Abstract

The principal author reports here the main elements of work performed as part of his 1999 Ph.D. dissertation (Matthew Keith West, ''Diffusion of Sulfur into Natural Diamond: Characterization and Applications in Radiation Detection''. Ph.D. Dissertation, University of Missouri-Columbia, USA (1999)). In this study a Field Enhanced Diffusion with Optical Activation (FEDOA) reactor was constructed, tested, and employed to diffuse sulfur and sodium into polished, natural diamond plates. Various chemical sources of sulfur were used for diffusion from the gaseous, liquid, and solid phases. Diffusion coefficients in the range of 10 � 15 cm 2 /s to 10 � 14 cm 2 /s for temperatures 450-1050 � C, have been calculated for sulfur from concentration profiles determined from secondary ion mass spectroscopy (SIMS) analysis. Sulfur demonstrated n-type behavior with an activation energy of 0.9 eV. Sodium was found to diffuse into diamond with an average diffusion coefficient of 7.2 � 10 � 14 cm 2 /s at 750 � C. The different sources of sulfur provided qualitative information about competing mechanisms in the diffusion process.
硫和钠:潜在供体在天然钻石中的扩散
主要作者在这里报告了他1999年博士论文(Matthew Keith West,“硫在天然钻石中的扩散:辐射探测中的表征和应用”)中所做的主要工作。博士学位论文,美国密苏里大学哥伦比亚分校(1999)。在这项研究中,我们构建了一个光活化场增强扩散反应器(FEDOA),测试并使用它将硫和钠扩散到抛光的天然金刚石片中。硫的各种化学来源被用于从气态、液态和固相扩散。从二次离子质谱(SIMS)分析确定的硫浓度曲线中,计算出温度为450-1050℃时,扩散系数范围为10 - 15 cm 2 /s至10 - 14 cm 2 /s。硫表现为n型行为,活化能为0.9 eV。在750℃时,钠扩散到金刚石中的平均扩散系数为7.2 ~ 10 ~ 14 cm 2 /s。不同来源的硫提供了扩散过程中竞争机制的定性信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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