Abstract. Oxygenated organic molecules (OOMs) are the crucial intermediates linking
volatile organic compounds (VOCs) to secondary organic aerosols (SOAs) in the
atmosphere, but comprehensive understanding of the characteristics of OOMs
and their formation from VOCs is still missing. Ambient observations of
OOMs using recently developed mass spectrometry techniques are still
limited, especially in polluted urban atmospheres where VOCs and oxidants are
extremely variable and complex. Here, we investigate OOMs, measured by a
nitrate-ion-based chemical ionization mass spectrometer at Nanjing in
eastern China, through performing positive matrix factorization on binned
mass spectra (binPMF). The binPMF analysis reveals three factors about
anthropogenic VOC (AVOC) daytime chemistry, three isoprene-related
factors, three factors about biogenic VOC (BVOC) nighttime chemistry, and
three factors about nitrated phenols. All factors are influenced by NOx
in different ways and to different extents. Over 1000 non-nitro molecules
have been identified and then reconstructed from the selected solution of
binPMF, and about 72 % of the total signals are contributed by
nitrogen-containing OOMs, mostly regarded as organic nitrates formed through
peroxy radicals terminated by nitric oxide or nitrate-radical-initiated
oxidations. Moreover, multi-nitrates account for about 24 % of the total
signals, indicating the significant presence of multiple generations,
especially for isoprene (e.g., C5H10O8N2 and
C5H9O10N3). Additionally, the distribution of OOM
concentration on the carbon number confirms their precursors are driven by AVOCs
mixed with enhanced BVOCs during summer. Our results highlight the decisive
role of NOx in OOM formation in densely populated areas, and we encourage
more studies on the dramatic interactions between anthropogenic and biogenic
emissions.