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Hydrogen trapping and stability at the polycrystalline CVD diamond surface and in the subsurface layers

机译:多晶CVD金刚石表面和地下层的氢捕获和稳定性

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Diffusion profiles, effusion and x-ray photoelectron spectroscopy experiments are performed on hydrogenated (deuterated) CVD polycrystalline diamond in order to study the location and stability of hydrogen at the diamond surface and in the subsurface layers. The samples, as-grown with deuterium or submitted to deuterium plasma, are then annealed and chemically etched. A thermal treatment at 600 °C modifies the concentration of deuterium accumulated in the subsurface region, while this is not observed by simple chemical etching. The effusion spectra obtained after thermal and chemical treatments show that hydrogen trapped in the subsurface layers is stable up to 700 °C and that the chemical treatment leads to decrease the effusion peak at 860 °C, i.e. the hydrogen trapped at the unface. X-ray photoelectron spectroscopy analyses reveal the evolution of carbon bonding from sp~2 to sp~3. The compete sp~3 bonding is reached after annealing and etching, or after annealing up to 950 °C.
机译:扩散轮廓,积分和X射线光电子能谱实验在氢化(氘代)CVD多晶硅金刚石上进行,以研究金刚石表面和地下层的氢的位置和稳定性。然后用退火和化学蚀刻的用氘生长或用氘生长或提交至氘血浆。在600℃下的热处理改变了在地下区域中累积的氘的浓度,而通过简单的化学蚀刻未观察到这一点。热和化学处理后获得的活力谱表明,捕获在地下层中的氢气稳定至700℃,并且化学处理导致860℃下的积液峰值降低,即捕获在UNFACE处的氢气。 X射线光电子能谱分析显示从SP〜2至SP〜3的碳键合的演变。在退火和蚀刻后达到竞争SP〜3键合,或者在最高可达950°C后达到。

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