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Hot-filament diamond deposition with sulfur addition

机译:添加硫磺的热丝金刚石沉积

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To understand the action of sulfur additions during low-pressure, diamond deposition experiments were carried out in a hot-filament apparatus. As a sulfur compound, H{sub}2S was used and diamond growth was studied for various sulfur additions between 400 and 2200 ppm H{sub}2S/CH{sub}4. To get further information about the interactions of the sulfur compounds during deposition, the deposition parameters substrate temperature and filament temperature were varied. Thermodynamic calculations showed that H{sub}2S reacts with methane to the compound CS during filament activation. At the substrate temperature for diamond deposition (< 1000 ℃) there should be the reverse reaction from CS to H{sub}2S. It could be shown that sulfur reduces the diamond growth rate during the period of nucleation and individual crystal growth. After a diamond layer has been formed, the diamond growth rate increases to values higher than in the undoped system. This can be explained by an additional carbon transport due to the formed CS.
机译:为了了解添加硫在低压下的作用,在热丝设备中进行了金刚石沉积实验。使用H {sub} 2S作为硫化合物,并研究了400至2200 ppm H {sub} 2S / CH {sub} 4之间各种硫磺添加量的金刚石生长。为了获得有关硫化合物在沉积过程中相互作用的更多信息,改变沉积参数的衬底温度和灯丝温度。热力学计算表明,H {sub} 2S在灯丝活化过程中与甲烷反应生成化合物CS。在金刚石沉积的底物温度(<1000℃)下,应该有从CS到H {sub} 2S的逆反应。可以证明,在成核和单个晶体生长期间,硫降低了金刚石的生长速率。在形成金刚石层之后,金刚石生长速率增加到比未掺杂系统中更高的值。这可以通过形成的CS进行额外的碳传输来解释。

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