论文标题
在实验室条件下的硅和氢化学模仿进化恒星的大气
Silicon and hydrogen chemistry under laboratory conditions mimicking the atmosphere of evolved stars
论文作者
论文摘要
硅存在于星际粉尘颗粒,陨石和小行星中,至今已在气相中检测到13个含硅的分子,朝着晚期恒星或分子云(包括硅烷和硅烷衍生物)中检测到。在这项工作中,我们在实验中研究了原子硅和氢之间的相互作用,这些物理条件模仿了进化恒星大气的人。我们发现,Si,h和h $ _2 $的化学反应有效地产生硅烷(SIH $ _4 $),DISILANE(SI $ _2 $ _2 $ H $ _6 $)和无定形的氢化硅(A-SI:H)晶粒。 Silane肯定已被检测到富含碳富含碳的IRC \,+10216,而在太空中尚未检测到DiSilane。因此,根据我们的结果,我们建议原子Si与H和H $ _2 $的气相反应是富含C的AGB中硅烷的合理来源,尽管它对SIH $ _4 $丰度的总贡献可能很低,而与暗示的形成途径相比,通过对尘埃颗粒表面的催化反应相比。此外,在500 K以上的温度下,生产的A-SI:H粉尘类似物分解为SIH $ _4 $和SI $ _2 $ _2 $ H $ _6 $,这表明在进化星周围的信封中形成这些物种的附加机制。我们还发现,这些粉尘类似物对水蒸气的暴露会导致将氧气掺入Si-O-SI和Si-OH组中,而以SIH部分为代价,这意味着,如果这种类型的谷物存在于星际介质中,则可能会通过与水面覆盖地表的水面相互作用将它们处理成硅质,从而将它们加工成硅胶中。
Silicon is present in interstellar dust grains, meteorites and asteroids, and to date thirteen silicon-bearing molecules have been detected in the gas-phase towards late-type stars or molecular clouds, including silane and silane derivatives. In this work, we have experimentally studied the interaction between atomic silicon and hydrogen under physical conditions mimicking those at the atmosphere of evolved stars. We have found that the chemistry of Si, H and H$_2$ efficiently produces silane (SiH$_4$), disilane (Si$_2$H$_6$) and amorphous hydrogenated silicon (a-Si:H) grains. Silane has been definitely detected towards the carbon-rich star IRC\,+10216, while disilane has not been detected in space yet. Thus, based on our results, we propose that gas-phase reactions of atomic Si with H and H$_2$ are a plausible source of silane in C-rich AGBs, although its contribution to the total SiH$_4$ abundance may be low in comparison with the suggested formation route by catalytic reactions on the surface of dust grains. In addition, the produced a-Si:H dust analogs decompose into SiH$_4$ and Si$_2$H$_6$ at temperatures above 500 K, suggesting an additional mechanism of formation of these species in envelopes around evolved stars. We have also found that the exposure of these dust analogs to water vapor leads to the incorporation of oxygen into Si-O-Si and Si-OH groups at the expense of SiH moieties, which implies that, if this type of grains are present in the interstellar medium, they will be probably processed into silicates through the interaction with water ices covering the surface of dust grains.