Methane formation in cold regions from carbon atoms and molecular hydrogen
arXiv:2110.15881 · doi:10.3847/1538-4357/ac51d1
Abstract
Methane is typically thought to be formed in the solid state on the surface of cold interstellar icy grain mantles via the successive atomic hydrogenation of a carbon atom. In the current work we investigate the potential role of molecular hydrogen in the CH reaction network. We make use of an ultra-high vacuum cryogenic setup combining an atomic carbon atom beam and both atomic and/or molecular beams of hydrogen and deuterium on a HO ice. These experiments lead to the formation of methane isotopologues detected in situ through reflection absorption infrared spectroscopy. Most notably, CH is formed in an experiment combining C atoms with H on amorphous solid water, albeit slower than in experiments with H atoms present. Furthermore, CHD is detected in an experiment of C atoms with H and D on HO ice. CD, however, is only formed when D atoms are present in the experiment. These findings have been rationalized by means of computational chemical insights. This leads to the following conclusions: a) the reaction C + H -> CH can take place, although not barrierless in the presence of water, b) the reaction CH + H -> CH is barrierless, but has not yet been included in astrochemical models, c) the reactions CH + H -> CH + H and CH + H -> CH + H can take place only via a tunneling mechanism and d) molecular hydrogen possibly plays a more important role in the solid-state formation of methane than assumed so far.
Submitted to ApJ
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