4.7 Article

Fates of secondary organic aerosols in the atmosphere identified fromcompound-specific dual-carbon isotope analysis of oxalic acid

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 23, Issue 2, Pages 1565-1578

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-23-1565-2023

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This study investigates the fate of SOAs in the atmosphere using a novel compound-specific dual-carbon isotope fingerprinting technique. Results show that photochemical aging and aqueous-phase chemical processes dominate the formation of oxalic acid in summer and winter, respectively. The study also highlights the spatial and seasonal variations in SOA carbon sources and chemical processes, emphasizing the importance of including these variations in climate projection models and air quality management practices in China.
Secondary organic aerosols (SOAs) are important components of fine particulates in the atmosphere. However, the sources of SOA precursor and atmospheric processes affecting SOAs are poorly understood. This limits our abilities to improve air quality and model aerosol-mediated climate forcing. Here, we use novel compound-specific dual-carbon isotope fingerprints (delta C-14 and delta C-13) for individual SOA tracer molecules (i.e., oxalic acid) to investigate the fates of SOAs in the atmosphere at five emission hotspots in China. Coal combustion and vehicle exhaust accounted for similar to 55 % of the sources of carbon in oxalic acid in Beijing and Shanghai, but biomass burning and biogenic emissions accounted for similar to 70 % of the sources of carbon in oxalic acid in Chengdu, Guangzhou, and Wuhan during the sampling period. The dual-carbon isotope signatures of oxalic acid and bulk organic carbon pools (e.g., water-soluble organic carbon) were compared to investigate the fates of SOAs in the atmosphere. Photochemical aging and aqueous-phase chemical processes dominate the formation of oxalic acid in summer and in winter, respectively. The results indicated that SOA carbon sources and chemical processes producing SOAs vary spatially and seasonally, and these variations need to be included in Chinese climate projection models and air quality management practices.

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