One year online measurements of water-soluble ions at the industrially polluted town of Nanjing, China: Sources, seasonal and diurnal variations

被引:70
|
作者
Wang, Honglei [1 ]
An, Junlin [1 ]
Cheng, Mengtian [2 ]
Shen, Lijuan [3 ]
Zhu, Bin [1 ]
Li, Yi [4 ]
Wang, Yuesi [2 ]
Duan, Qing [1 ]
Sullivan, Amy [4 ]
Xia, Li [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Key Lab Aerosol Cloud Precipitat, China Meteorol Adm, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing 210044, Jiangsu, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[3] Jiaxing Environm Monitoring Stn, Jiaxing 314000, Peoples R China
[4] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
基金
中国国家自然科学基金;
关键词
Water-soluble ions; RCFP-IC; PCA/APCS; Haze; Diurnal variation; Source; YANGTZE-RIVER DELTA; SECONDARY INORGANIC AEROSOL; SOURCE APPORTIONMENT; AIR-POLLUTION; CHEMICAL-CHARACTERIZATION; PRECURSOR GASES; EASTERN CHINA; ACIDIC GASES; PM2.5; PARTICLES;
D O I
10.1016/j.chemosphere.2016.01.066
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Half-hourly mass concentrations water-soluble ions (WSIs) and PM2.5 were measured online a Rapid Collector of Fine Particles and Ion Chromatography system (RCFP-IC) and FH62C14 Continuous Particulate Monitor in Nanjing from October 18, 2013 to November 17, 2014. The WSIs concentration ranged from 7.07 to 333.42 mu g m(-3) with an annual mean of 76.32 mu g m(-3). The WSIs ranked in the order of SO42- > NH4+ > NO3- > Cl- > NO2- > K+ > Ca2+ > Na+ > Mg2+. The PM2.5 concentration ranged from 4.00 to 400 mu g m(-3) with an annual mean of 83.58 mu g m(-3). The concentrations of WSIs varied in the order of winter (115.77 mu g m(-3)) > spring (76.10 mu g m(-3)) > autumn (63.72 mu g m(-3)) > summer (59.75 mu g m(-3)), with the highest level in January (123.99 mu g m(-3)) and lowest level in August (43.73 mu g m(-3)). Different WSIs had distinct diurnal variations. The source analysis of the WSIs in the PCA/APCS mode illustrated that the sources consisted of secondary aerosol, coal combustion, mineral dust, biomass burning, traffic emissions and sea salt. In addition, there were seasonal variations amongst the various sources. The haze formation mechanism was different in summer and winter. The winter was dominated by NH4NO3 (18.56%), (NH4)(2)SO4 (28.63%), NH4+ (11.27%), SO42- (18.35%) and NO3- (13.13%), and by NH3 (25.93%), (NH4)(2)SO4 (13.37%), SO42- (15.74%) and NO3- (9.97%) in summer. Consequently, the proportions of HCl, HNO3, NH4+, SO42- and NO3- were much larger during haze episodes in winter, while it was dominated by NH4NO3, NH4+, (NH4)(2)SO4, SO42- and NO3- during summer haze episodes. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:526 / 536
页数:11
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