Abstract
Oxidative potential (OP) is increasingly recognized as a more health-relevant metric than particulate matter (PM) mass concentration because of its response to varying chemical compositions. Given the limited research on the OP of complex combustion aerosols, the effects of aging processes on their OP remain underexplored. We used online instruments to track the evolution of OP [via dithiothreitol (DTT) assays] during the aging of wood burning and coal combustion emissions by hydroxyl-radical-driven photooxidation and dark ozonolysis. We observed very substantial increases in the intrinsic OP (OP(m) (DTT)) of complex combustion aerosols (e.g., OP(m) (DTT) up to 100 pmol min(-1) μg(-1) for OH-aged wood burning emissions) within 1 day of equivalent aging. Further analysis in relation to the degree of oxidation revealed a potential for generalizing the OP of carbonaceous aerosols with average carbon oxidation state values ranging from -1.5 to -0.5 by assuming they have a constant OP(m) (DTT) value of ∼10 ± 6 pmol min(-1) μg(-1). Additionally, we uncovered a strong dependency of OP(m) (DTT) on both the source/precursor and aging pathway with above ∼-0.5. OH photooxidation was identified as an exceptionally efficient pathway for generating highly oxidized, multifunctionalized, and DTT-active products, particularly from wood burning emissions.