To better understand the origins and seasonality of atmospheric aerosols in North China, we collected fine aerosols (PM2.5) at an urban site (Nankai District, ND) and a suburban site (Haihe Education Park, HEP) in Tianjin from July 2018 to July 2019. The PM2.5 was studied for carbonaceous, nitrogenous and ionic components and stable carbon and nitrogen isotope ratios of total carbon (δ13CTC) and nitrogen (δ15NTN). On average, the mass concentrations of PM2.5, organic carbon (OC), elemental carbon (EC) and water-soluble OC (WSOC) were higher in winter than in summer at both ND and HEP. SO, NO and NH were the dominant ions, and their sum accounted for 89 % of the total ionic mass at ND and 87 % at HEP. NO and NH peaked in winter and were at their minimum in summer, whereas SO was higher in summer than in all the other seasons at HEP and was comparable among the seasons, although it peaked in winter at ND. δ13CTC and δ15NTN were −26.5 ‰ to −21.9 ‰ and +1.01 ‰ to +22.8 ‰ at ND and −25.5 ‰ to −22.8 ‰ and +4.91 ‰ to +18.6 ‰ at HEP. Based on seasonal variations in the measured parameters, we found that coal and biomass combustion emissions are the dominant sources of PM2.5 in autumn and winter, while terrestrial and/or marine biological emissions are important in spring and summer in the Tianjin region, North China. In addition, our results implied that the secondary formation pathways of secondary organic aerosols in autumn/winter were different from those in spring/summer; i.e., they might be driven by NO3 radicals in the former period.
Figure 1. Temporal variations in δ13CTC and δ15NTN and concentrations of PM2.5 and its chemical components OC, EC, WSOC and SOC at ND (solid dots) and HEP (solid stars) in Tianjin during 2018–2019.
Citation: Dong, Z., Pavuluri, C. M., Xu, Z., Wang, Y., Li, P., Fu, P., and Liu, C.-Q.: Measurement report: Chemical components and 13C and 15N isotope ratios of fine aerosols over Tianjin, North China: year-round observations, Atmos. Chem. Phys., 2023, 23, 2119–2143. https://doi.org/10.5194/acp-23-2119-2023.
