Oxygenated organic molecules (OOMs) are dominated by the N-containing species in polluted urban environments. As N-containing OOMs, especially those with more than one nitrogen atom, prevail in the high inline-formula
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(mass-to-charge) range (inline-formula
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350 Th), unambiguous identification of N-containing OOMs is highly desirable for understanding of their formation processes, precursors and influencing factors. To achieve this, we applied an ultra-high-resolution chemical-ionization Orbitrap (CI-Orbitrap) in a field campaign and found that OOMs contain one (1N-OOMs), two (2N-OOMs) and three (3N-OOMs) nitrogen atoms comprised 50 %, 26 % and 4 %, respectively, of total OOMs. More interestingly, the fraction of 2N-OOMs increased with the increase in carbon number (nC) and was dominated by the ones derived from aliphatic precursors (2N-OOMinline-formulaAli, 64.2 %), indicating the importance of multistep oxidation. Plausible precursors of 2N-OOMs were aliphatics (2N-OOMinline-formulaAli, 64.2 %), aromatics (2N-OOMinline-formulaAro, 16 %) and monoterpenes (2N-OOMinline-formulaMT, 15.4 %). The absolute concentrations of 2N-OOMs were greatly affected by the pollution level for most cases. The 2N-OOMinline-formulaAli was the most abundant 2N-OOM, and its fraction even increased on the polluted day with an enhanced proportion of the ones with nC inline-formula>10. While 2N-OOMinline-formulaAli and 2N-OOMinline-formulaAro were dominated by daytime photochemical production, nighttime NOinline-formula3-initiated oxidation played a comparable role to the daytime photochemistry in the formation of 2N-OOMinline-formulaMT. The 2N-OOMinline-formulaAro species were of the highest oxygenation level, followed by 2N-OOMinline-formulaMT and 2N-OOMinline-formulaAli, which were affected by photochemistry and NOinline-formulax concentrations. These results highlight the significant formation of 2N-OOMs and the influencing factors on their formation in polluted urban environments, where various volatile organic compound (VOC) precursors and atmospheric oxidants are present.