Imidazole produced by the interaction of glyoxal with
nitrogen-containing
chemicals in atmospheric particles can yield secondary organic aerosol
(SOA) due to atmospheric oxidation. However, knowledge about the aqueous
phase reaction mechanism of imidazole formation and its oxidation
is still very limited. This work investigated the formation mechanism
and aqueous-phase oxidative degradation reactions of imidazole with
the hydroxyl radical (•OH), nitrate radical (NO3
•), and ozone (O3). Results showed
that the formation of imidazole involves many dehydration reactions
and is favorable under moderate- or low-RH conditions. The calculated
atmospheric lifetimes of 14.05, 0.27, and 3.45 h for reactions with •OH, NO3
•, and O3, respectively, suggest the efficient oxidation of imidazole under
tropospheric aqueous-phase conditions. Formamide and oxamide are the
main products in the presence of O2, and nitro-imidazoles
can also be formed in the presence of NO2. The optical
properties of imidazole evolve significantly, attributable to the
formation of nitro-imidazoles, resulting in a red shift of absorption
peak to the UVA and UVB region.