Chemical Characteristics and Sources of Water-Soluble Organic Nitrogen Species in PM2.5 in Nanjing, China

• Published in: Atmosphere 2021-05, Vol.12 (5), p.574
• Main Authors: Liu, Yue, Li, Haiwei, Cui, Shijie, Nie, Dongyang, Chen, Yanfang, Ge, Xinlei
• Format: Article
• Language: English
• Subjects: Aerosols; Air quality; Amines; Ammonium; Ammonium compounds; aqueous-phase oxidation; Biomass burning; Burning; Carbon; Components; Correlation analysis; Hydrocarbons; Mass; mass spectra; Mass spectrometry; Nitrates; Nitrogen; Organic matter; Organic nitrogen; Oxidation; Particulate matter; Photochemicals; Photochemistry; Soot; source apportionment; Suburban areas; Summer; Temporal variations; Water chemistry; Winter
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos12050574

Water-soluble organic nitrogen (WSON) is an important component of PM2.5 which may affect air quality, climate and human health. Herein, one-year field samples of atmospheric PM2.5 (June 2017–May 2018) were collected in northern Nanjing. Chemical characterization of PM2.5 major components as well as WSON were conducted, and WSON composition and sources were further investigated via measurements by a Aerodyne soot particle aerosol mass spectrometer (SP-AMS) as well as positive matrix factorization (PMF). Inorganic ions, mainly consisting of ammonium, sulfate, and nitrate, were found to dominate PM2.5 mass (58.7%), followed by organic matter (OM) (22.6%), and elemental carbon (EC) (2.1%). Water-soluble OM dominated OM (65.1%), and its temporal variation was closely correlated with that of secondary organic matter, while time series of water-insoluble OM concentrations correlated tightly with that of primary organic matter. Average WSON concentration was 2.15 μg/m3, which was highest in winter and lowest in summer. Correlation analysis of WSON with PM2.5 components also indicated that WSON was mainly from secondary sources. SP-AMS revealed that WSON mass spectrum was composed of CxHyNp+ (91.2%) and CxHyOzNp+ (8.8%), indicating dominance of amines and other oxygenated ON compounds. PMF analysis resolved two primary sources (traffic, biomass burning) and two secondary sources (less-oxidized and more-oxidized factors) of WSOM and WSON, and the secondary source dominated both WSOM and WSON. Contribution of the more-oxidized ON factor was very high in winter, and the less-oxidized factor was significant in summer, indicating a likely important role of aqueous-phase processing in winter as well as photochemical oxidation in summer to WSON.