Chemical composition, sources and evolution processes of aerosol at an urban site in Yangtze River Delta, China during wintertime

被引:63
作者
Zhang, Yunjiang [1 ,2 ]
Tang, Lili [1 ,2 ]
Yu, Hongxia [3 ]
Wang, Zhuang [1 ]
Sun, Yele [4 ]
Qin, Wei [2 ]
Chen, Wentai [2 ]
Chen, Changhong [5 ]
Ding, Aijun [6 ,7 ]
Wu, Jing [1 ]
Ge, Shun [2 ]
Chen, Cheng [2 ]
Zhou, Hong-cang [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Sch Environm Sci & Engn, Jiangsu Key Lab Atmospher Environm Monitoring & P, Nanjing 210044, Jiangsu, Peoples R China
[2] Jiangsu Environm Monitoring Ctr, Nanjing 210036, Jiangsu, Peoples R China
[3] Nanjing Univ, Sch Environm, State Key Lab Pollut Control & Resource Reuse, Nanjing 210093, Jiangsu, Peoples R China
[4] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[5] Shanghai Acad Environm Sci, Shanghai 200233, Peoples R China
[6] Nanjing Univ, Inst Climate & Global Change Res, Nanjing 210093, Jiangsu, Peoples R China
[7] Nanjing Univ, Sch Atmospher Sci, Nanjing 210093, Jiangsu, Peoples R China
基金
中国国家自然科学基金;
关键词
Haze; PM1; Components; Sources; Evolution processes; YRD; POSITIVE MATRIX FACTORIZATION; FINE-PARTICLE COMPOSITION; MASS-SPECTROMETER DATA; ORGANIC AEROSOLS; SOURCE APPORTIONMENT; SUBMICRON AEROSOLS; SPECIATION MONITOR; MEXICO-CITY; RURAL SITE; EMISSIONS;
D O I
10.1016/j.atmosenv.2015.08.017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To investigate the composition, sources and evolution processes of submicron aerosol during wintertime, a field experiment was conducted during December 1-31, 2013 in urban Nanjing, a megacity in Yangtze River Delta of China. Non-refractory submicron aerosol (NR-PM1) species were measured with an Aerodyne Aerosol Chemical Speciation Monitor. NR-PM1 is dominated by secondary inorganic aerosol (55%) and organic aerosol (OA, 42%) during haze periods. Six OA components were identified by positive matrix factorization of the OA mass spectra. The hydrocarbon-like OA and cooking-related OA represent the local traffic and cooking sources, respectively. A highly oxidized factor related to biomass burning OA accounted for 15% of the total OA mass during haze periods. Three types of oxygenated OA (OOA), i.e., a less-oxidized OOA (LO-OOA), a more-oxidized OOA (MO-OOA), and a low-volatility OOA (LV-OOA), were identified. LO-OOA is likely associated with fresh urban secondary OA. MO-OOA likely represents photochemical products showing a similar diurnal cycle to nitrate with a pronounced noon peak. LV-OOA appears to be a more oxidized factor with a pronounced noon peak. The OA composition is dominated by secondary species, especially during haze events. LO-OOA, MO-OOA and LV-OOA on average account for 11%, (18%), 24% (21%) and 23% (18%) of the total OA mass for the haze (clean) periods respectively. Analysis of meteorological influence suggested that regional transport from the northern and southeastern areas of the city is responsible for large secondary and low-volatility aerosol formation. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:339 / 349
页数:11
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