Abstract. For the first time in the North China Plain (NCP) region, we
investigated the seasonal variations in submicron particles (NR-PM1)
and their chemical composition at a background mountainous site of Xinglong
using an Aerodyne high-resolution time-of-flight aerosol mass spectrometer. The average concentration of NR-PM1 was highest in autumn (15.1 µg m−3) and lowest in summer (12.4 µg m−3), with a greater abundance of nitrate in spring (34 %), winter (31 %) and autumn (34 %) and elevated organics (40 %) and sulfate (38 %) in summer. PM1 in Xinglong showed higher acidity in summer and moderate acidity in spring, autumn and winter, with average pH values of 2.7±0.6, 4.2±0.7, 3.5±0.5 and 3.7±0.6, respectively, which is higher than those estimated in the United States and Europe. The size distribution of all PM1 species showed a consistent accumulation mode peaking at approximately 600–800 nm (dva), indicating a highly aged and internally mixed nature of the background aerosols, which was further supported by the source appointment results using positive matrix factorization and multilinear engine analysis. Significant contributions of aged secondary organic aerosol (SOA) in organic aerosol (OA) were resolved in all seasons (>77 %), especially in summer. The oxidation state and the process of evolution of OAs in the four seasons were further investigated, and an enhanced carbon oxidation state (−0.45–0.10) and O/C (0.54–0.75) and OM/OC (1.86–2.13) ratios – compared with urban
studies – were observed, with the highest oxidation state appearing in
summer, likely because of the relatively stronger photochemical processing
that dominated the formation processes of both less oxidized OA (LO-OOA) and
more oxidized OA (MO-OOA). Aqueous-phase processing also contributed to the
SOA formation and prevailed in winter, with the share to MO-OOA being more
important than that to LO-OOA. In addition, regional transport also played
an important role in the variations in SOA. Especially in summer,
continuous increases in SOA concentration as a function of odd oxygen (Ox=O3+NO2) were found to
be associated with the increases in wind speed. Furthermore, backward
trajectory analysis showed that higher concentrations of submicron
particles were associated with air masses transported short distances
from the southern regions in all four seasons, while long-range transport
from Inner Mongolia (western and northern regions) also contributed to
summertime particulate pollution in the background areas of the NCP. Our
results illustrate that the background particles in the NCP are influenced
significantly by aging processes and regional transport, and the increased
contribution of aerosol nitrate highlights how regional reductions in
nitrogen oxide emissions are critical for remedying occurrence of
nitrate-dominated haze events over the NCP.