Abstract. Nitrogen-containing organic compounds (NOCs) substantially contribute to
light-absorbing organic aerosols, although the atmospheric processes
responsible for the secondary formation of these compounds are poorly
understood. In this study, seasonal atmospheric processing of NOCs is
investigated using single-particle mass spectrometry in urban Guangzhou from
2013 to 2014. The relative abundance of NOCs is found to be strongly enhanced
when they are internally mixed with photochemically produced secondary oxidized
organics (i.e., formate, acetate, pyruvate, methylglyoxal, glyoxylate,
oxalate, malonate, and succinate) and ammonium (NH4+). Moreover, both the hourly
detected particle number and the relative abundance of NOCs are highly
correlated with those of secondary oxidized organics and NH4+. Therefore, it is hypothesized that the secondary formation of NOCs is most likely linked to oxidized organics and NH4+. Results from both multiple linear
regression analysis and positive matrix factorization analysis further show
that the relative abundance of NOCs could be well predicted (R2 > 0.7, p < 0.01) by oxidized organics and NH4+. Interestingly, the relative abundance of NOCs is inversely correlated with
NH4+, whereas their number fractions are positively correlated. This
result suggests that although the formation of NOCs does require the
involvement of NH3/NH4+, the relative amount of NH4+ may have
a negative effect. Higher humidity and NOx likely facilitates the conversion
of oxidized organics to NOCs. Due to the relatively high oxidized organics
and NH3/NH4+, the relative contributions of NOCs in summer and
fall were higher than those in spring and winter. To the best of our
knowledge, this is the first direct field observation study reporting a
close association between NOCs and both oxidized organics and NH4+.
These findings have substantial implications for the role of NH4+ in the
atmosphere, particularly in models that predict the evolution and deposition
of NOCs.Highlights.
NOCs were highly internally mixed with photochemically produced secondary oxidized organics NOCs could be well predicted by the variations of these oxidized organics
and NH4+ Higher relative humidity and NOx may facilitate the conversion of these
oxidized organics to NOCs