二硅烷
硅烷
硅烷
硅
沉积(地质)
脱氢
非晶硅
化学
碎片(计算)
等离子体
无定形固体
纳米技术
化学工程
晶体硅
材料科学
结晶学
有机化学
催化作用
物理
地质学
计算机科学
操作系统
古生物学
量子力学
沉积物
工程类
标识
DOI:10.1016/0040-6090(89)90819-5
摘要
The originally proposed mechanism of plasma-induced deposition of silicon from silane via the SiH3 radical, as suggested by several research groups, was based on speculation rather than on facts. Critical consideration of the experimental facts which were published recently shows that there is no substantial evidence for this reaction channel, and that the possible contribution of the SiH3 radical to the generally observed deposition rate of amorphous silicon (a-Si) and crystalline silicon (c-Si) is negligible. Based on the experimental data available so far it is shown that the most probable dominant reaction channel involves, as a first step, the fragmentation of silane into SiH2 and H2. In the case of a-Si deposition, this is followed by rapid formation of disilane (and to lesser extent higher silanes) which then decomposes at the surface of the growing film. The deposition of c-Si involves a direct insertion of SiH2 into the surface of the growing film. The ion-impact-induced dehydrogenation of the surface is the rate-determining step for fast growth rates.
科研通智能强力驱动
Strongly Powered by AbleSci AI