Abstract

AbstractInteractions between proteinaceous matter and atmospheric oxidants can affect amino acids (AAs) bioavailability, the climate, and human health. However, atmospheric reactions of proteinaceous matter remain poorly understood. PM2.5 samples were collected during spring (2019) and winter (2020) sampling campaigns conducted in Nanchang, China. Concentrations of combined and free AAs, and the δ15N values of combined and free glycine (C‐Gly and F‐Gly) in PM2.5 samples were analyzed. Concentrations of TFAA under different O3 and NO2 levels, and correlations of specific FAA species with ambient O3 and NO2 concentrations suggest that the ability of O3 to release TFAA from proteinaceous matter is greater than that of NO2. Furthermore, O3 may trend to release neutral and hydrophilic FAA species, whereas NO2 tends to generate hydrophobic FAA species. With aerosol aging, the slope of the fitted line between [TFAA] and [TSAA] [O3 + NO2] increased, indicating that FAAs yield from protein degradation in PM2.5 was affected greatly by aerosol aging. The TCAAs concentration observed in spring was substantially higher than that in winter. Moreover, the δ15NF‐Gly and δ15NC‐Gly values in PM2.5 exhibited negative correlations with atmospheric O3 concentration. These results suggest that increased levels of proteinaceous matter in spring were derived from natural sources related to biological activities rather than biomass burning sources. Our study confirms that the reaction of degradation of proteinaceous matter to FAAs could be influenced by aerosol aging, which is a finding that enhances current understanding regarding atmospheric processes of aerosol proteinaceous matter under different ambient O3 and NO2 levels.

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