Abstract. Secondary organic aerosol (SOA) plays an important role in particulate air
pollution, but its formation mechanism is still not fully understood. The
chemical composition of non-refractory particulate matter with a diameter
≤2.5 µm (NR-PM2.5), OA sources, and SOA formation
mechanisms were investigated in urban Xi'an during winter 2018. The
fractional contribution of SOA to total OA mass (58 %) was larger than
primary OA (POA, 42 %). Biomass-burning-influenced oxygenated OA
(OOA-BB) was resolved in urban Xi'an and was formed from the
photochemical oxidation and aging of biomass burning OA (BBOA). The
formation of OOA-BB was more favorable on days with a larger OA fraction
and higher BBOA concentration. In comparison, the aqueous-phase processed
oxygenated OA (aq-OOA) was more dependent on the secondary inorganic aerosol
(SIA) content and aerosol liquid water content (ALWC), and it showed a large increase
(to 50 % of OA) during SIA-enhanced periods. Further van Krevelen (VK)
diagram analysis suggests that the addition of carboxylic acid groups with
fragmentation dominated OA aging on reference days, while the increased
aq-OOA contributions during SIA-enhanced periods likely reflect OA evolution
due to the addition of alcohol or peroxide groups.