Photolysis of α-KETO Acids in Model Atmospheric Water

Recent work has reported the potential of aqueous-phase photochemistry to promote secondary organic aerosol (SOA) formation. New aqueous photochemical SOA sources may contribute to bridging the gap between field measurements of SOA and models of SOA formation. The ubiquitous α-ketocarboxylic acids pyruvic and glyoxylic acid are known products of the atmospheric oxidation of polycyclic aromatic hydrocarbons (PAHs) as well as of biogenic volatile organic compounds (VOCs). The combination of a carbonyl chromophore (absorbing at wavelengths λ ≥ 300 nm) and hydrophilic functional groups makes these acids likely candidates for forming aqueous SOA by direct sunlight photolysis. We use a variety of analytical techniques including: 2,4-dinitrophenylhydrazine (DNPH) derivatization; ultra-high performance liquid chromatography (UHPLC) and ion chromatography (IC) coupled to mass spectrometry;1H and 13C NMR; and 13C gCOSY NMR to probe the kinetics and mechanisms of the direct photolysis of model solutions of pyruvic acid and glyoxylic acid. The results indicate that despite the structural similarity between the two acids, they each react via very different primary photochemical pathways. Pyruvic acid undergoes a proton-coupled electron transfer (PCET) mechanism with radical recombination, resulting in CO2 and 6-8 carbon organic acids. In contrast, glyoxylic acid primarily undergoes α-cleavage to generate CO, CO2, and glyoxal which is a key species in SOA formation. This work demonstrates that aqueous photolysis is a very competitive atmospheric sink for both pyruvic and glyoxylic acid, indicating that these photoreactions are capable of contributing substantially to SOA formation.