Atmospheric chemistry of nitrogenous aerosols in northeastern Asia: biological sources and secondary formation

• Published in: Atmospheric chemistry and physics Vol. 15; no. 17; pp. 9883 - 9896
• Main Authors: Pavuluri, C M, Kawamura, K, Fu, P Q
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 02.09.2015; Copernicus Publications
• Subjects: Aerosols; Ageing; Aging; Air pollution; Atmospheric chemistry; Autumn; Biogeochemistry; Biological; Biomass; Biomass burning; Burning; Carbon; Carbonyl compounds; Carbonyls; Combustion; Emissions; Formations; Fossil fuels; Fuel combustion; Gases; Hydrocarbons; Isotope ratios; Nitrates; Nitrogen; Nitrogen (Chemical element); Nitrogen isotopes; Organic nitrogen; Pollution sources; Ratios; Seasonal variation; Seasonal variations; Seasonality; Spring; Spring (season); Summer; Suspended particulate matter; Terrestrial environments; Tracers; Water chemistry; Winter; Asia; Japan; Japan, Hokkaido, Sapporo; INW, Japan
• ISSN: 1680-7324; 1680-7316; 1680-7324
• DOI: 10.5194/acp-15-9883-2015

To better understand the sources of nitrogenous aerosols, particularly water-soluble organic nitrogen (WSON) and water-insoluble organic nitrogen (WION), in northeastern Asia, we measured total nitrogen (TN) and water-soluble total nitrogen (WSTN) as well as nitrogen isotope ratios ( delta 15N) of TN ( delta 15NTN) and WSTN ( delta 15NWSTN) in the total suspended particulate (TSP) samples collected from Sapporo, northern Japan, for a 1-year period. In general, WION was more abundant (126 plus or minus 117 ng m-3), whereas WSON was 89.7 plus or minus 80.6 ng m-3, accounting for 14 plus or minus 11 % and 9.2 plus or minus 7.3 % of TN, respectively. WSON peaked in late autumn to winter (maximum 288 ng m-3) and WION peaked in mid-spring to early summer (454 ng m-3). delta 15NTN (21.9 plus or minus 4.1 ppt) and delta 15NWSTN (25.8 plus or minus 8.2 ppt) showed peaks in summer with relatively high ratios in late autumn. Based on the seasonal variations in WSON and WION together with organic tracers, fossil fuel combustion and biomass burning are found to be two major sources of WSON, whereas emissions of biological particles and secondary formation by reactions of biogenic secondary organic species (carbonyls) with NH3 are suggested as an important source of WION. The seasonality of delta 15NTN and delta 15NWSTN, together with the comparisons to literature values, implies that chemical aging (including gas-particle partitioning) and biomass burning are the causes of the enhanced values in summer and autumn, respectively. This study demonstrates that contributions of aerosol N from fossil fuel combustion and biomass burning dominate in autumn and/or winter, whereas emission of terrestrial biological particles and secondary formation from biogenic hydrocarbons and subsequent chemical aging in the atmosphere are important in spring and/or summer in northeastern Asia.