The authors experimentally demonstrate that the major product of the reaction between CO and OH on ice surfaces is the HOCO radical, rather than CO2, which has been widely accepted as the predominant product. Using a novel Cs+ ion pickup technique, they quantify the branching ratio between HOCO and CO2 formation, finding that HOCO formation is at least 13 times more efficient than direct CO2 formation.
The traditional pathway for CO2 formation, CO + OH -> CO2 + H, has been reported to have low activation energies. However, the authors argue that these values align with the formation of HOCO rather than CO2, and a simple correction by substituting the products is needed to update astrochemical models.
The authors discuss the implications of their findings for interstellar ice chemistry. They suggest that future modeling efforts should incorporate the formation of HOCO and its subsequent reactions, such as HOCO + H -> CO2 + H2 and/or HCOOH, and HOCO + OH -> CO2 + H2O and/or H2CO3, instead of the direct CO2 formation pathway. They also highlight the need to consider nonthermal mechanisms for HOCO reactions, which can lift the temperature constraints for the formation of complex organic molecules in cold environments.
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