Theoretical analysis of the OH-initiated atmospheric oxidation reactions of imidazole.

Imidazoles are present in Earth's atmosphere in both the gas-phase and in aerosol particles, and have been implicated in the formation of brown carbon aerosols. The gas-phase oxidation of imidazole (CNH) by hydroxyl radicals has been shown to be preferentially initiated OH-addition to position C5, producing the 5-hydroxyimidazolyl radical adduct. However, the fate of this adduct upon reaction with O in the atmospheric gas-phase is currently unknown. We employed an automated approach to investigate the reaction mechanism and kinetics of imidazole's OH-initiated gas-phase oxidation, in the presence of O and NO. The explored mechanism included reactions available to first-generation RO radicals, as well as alkoxyl radicals produced from RO + NO reactions. Product distributions were obtained by assembling and solving a master equation, under conditions relevant to the Earth's atmosphere. Our calculations show a complex, branched reaction mechanism, which nevertheless converges to yield two major closed-shell products: 4-imidazol-4-ol (4-4ol) and ,'-diformylformamidine (FMF). At 298 K and 1 atm, we estimate the yields of 4-4ol and FMF from imidazole oxidation initiated OH-addition to position C5 to be 34 : 66, 12 : 85 and 2 : 95 under 10 ppt, 100 ppt and 1 ppb of NO respectively. This work also revealed O-migration pathways between the α--imino peroxyl radical isomers. This reaction channel is fast for the first-generation RO radicals, and may be important during the atmospheric oxidation of other unsaturated organic nitrogen compounds as well.