Water-soluble ions in atmospheric aerosols measured in five sites in the Yangtze River Delta, China: Size-fractionated, seasonal variations and sources

被引:78
作者
Wang, Honglei [1 ]
Zhu, Bin [1 ]
Shen, Lijuan [2 ]
Xu, Honghui [3 ]
An, Junlin [1 ]
Xue, Guoqiang [4 ]
Cao, Jinfei [5 ]
机构
[1] Nanjing Univ Informat Sci & Technol, China Meteorol Adm, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Key Lab Aerosol Cloud Precipitat, Nanjing 210044, Jiangsu, Peoples R China
[2] Jiaxing Environm Monitoring Stn, Jiaxing 314000, Peoples R China
[3] Zhejiang Inst Meteorol Sci, Hangzhou 310008, Zhejiang, Peoples R China
[4] Ningbo Meteorol Observ Zhejiang Prov, Ningbo 315012, Zhejiang, Peoples R China
[5] Suzhou Meteorol Observ Jiangsu Prov, Suzhou 215004, Peoples R China
基金
中国国家自然科学基金;
关键词
The Yangtze River Delta; Water-soluble ions; Seasonal distribution; Size distribution; Sources; INORGANIC-IONS; CHEMICAL-COMPOSITION; PARTICULATE MATTERS; FINE PARTICLES; HAZE POLLUTION; AIR-POLLUTION; MAJOR CITIES; URBAN SITES; PM2.5; SHANGHAI;
D O I
10.1016/j.atmosenv.2015.05.070
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In order to investigate the regional variations of water-soluble ions (WSIs), size-resolved measurement of aerosol particles and WSIs was conducted by using Anderson Sampler and Ion Chromatography at five sites (Nanjing, Suzhou, Lin'an, Hangzhou and Ningbo) in the Yangtze River Delta (YRD) region, China in the Autumn of 2012 and Winter, Spring and Summer of 2013. WSIs exhibited obvious seasonal variations due to the monsoon conversion, with the highest level in winter and lowest level in summer. The aerosol mass concentrations and WSIs in different size segments varied with four seasons. The dominant ions concentrations in PM2.1 ranked in the order of SO42- > NO3- > NH4+ > Cl- > K+> Ca2+, and the dominant ions concentrations in PM2.1 io ranked in the order of Ca2+ > NO3- > SO42- > Cl- > NH4+ > Na+. The size spectra of mass and WSIs concentration peaked mostly at 0.43-0.65 mu m in four seasons. The concentration discrepancies of WSIs in different cities were caused by the geographic locations and emission source. It's belonged to ammonium-rich distribution in PM2.1 and ammonium-poor distribution in PM2.1-10 in the YRD region. The impact of temperature on mass concentrations of NO3- and NH4+ in PM2.1 were stronger than those in PM2.1-10. PCA analysis shows that the sources of WSIs dominant by anthropogenic sources, soil particles or falling dust, sea salt and burning process. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:370 / 379
页数:10
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