Find in Library
Search millions of books, articles, and more
Indexed Open Access Databases
Chemical Characteristics and Sources of Water-Soluble Organic Nitrogen Species in PM<sub>2.5</sub> in Nanjing, China
oleh: Yue Liu, Haiwei Li, Shijie Cui, Dongyang Nie, Yanfang Chen, Xinlei Ge
Format: | Article |
---|---|
Diterbitkan: | MDPI AG 2021-04-01 |
Deskripsi
Water-soluble organic nitrogen (WSON) is an important component of PM<sub>2.5</sub> which may affect air quality, climate and human health. Herein, one-year field samples of atmospheric PM<sub>2.5</sub> (June 2017–May 2018) were collected in northern Nanjing. Chemical characterization of PM<sub>2.5</sub> 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 PM<sub>2.5</sub> 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/m<sup>3</sup>, which was highest in winter and lowest in summer. Correlation analysis of WSON with PM<sub>2.5</sub> components also indicated that WSON was mainly from secondary sources. SP-AMS revealed that WSON mass spectrum was composed of C<sub>x</sub>H<sub>y</sub>N<sub>p</sub><sup>+</sup> (91.2%) and C<sub>x</sub>H<sub>y</sub>O<sub>z</sub>N<sub>p</sub><sup>+</sup> (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.