Abstract. Nocturnal reactive nitrogen compounds play an important role in regional air
pollution. Here we present the measurements of dinitrogen pentoxide
(N2O5) associated with nitryl chloride (ClNO2) and particulate
nitrate (pNO3-) at a suburban site of Beijing in the summer of 2016.
High levels of N2O5 and ClNO2 were observed in the
outflow of the urban Beijing air masses, with 1 min average maxima of 937 and 2900 pptv,
respectively. The N2O5 uptake coefficients,
γ, and ClNO2 yield, f, were experimentally determined
from the observed parameters. The N2O5 uptake coefficient ranged
from 0.012 to 0.055, with an average of 0.034 ± 0.018, which is in the
upper range of previous field studies reported in North America and Europe
but is a moderate value in the North China Plain (NCP), which reflects
efficient N2O5 heterogeneous processes in Beijing. The
ClNO2 yield exhibited high variability, with a range of 0.50 to
unity and an average of 0.73 ± 0.25. The concentration of the nitrate
radical (NO3) was calculated assuming that the thermal equilibrium
between NO3 and N2O5 was maintained. In
NOx-rich air masses, the oxidation of nocturnal biogenic
volatile organic compounds (BVOCs) was dominated by NO3 rather than
O3. The production rate of organic nitrate (ON) via NO3 + BVOCs was
significant, with an average of 0.10 ± 0.07 ppbv h−1. We highlight
the importance of NO3 oxidation of VOCs in the formation of ON and
subsequent secondary organic aerosols in summer in Beijing.