Mixing and transformation of Asian dust with pollution in the two dust storms over the northern China in 2006

被引:48
作者
Zhang, Wenjie [2 ]
Zhuang, Guoshun [1 ]
Huang, Kan [1 ]
Li, Juan [1 ]
Zhang, Rong [1 ]
Wang, Qiongzhen [1 ]
Sun, Yele [4 ]
Fu, Joshua S. [5 ]
Chen, Ying [1 ]
Xu, Dongqun [3 ]
Wang, Wei [2 ]
机构
[1] Fudan Univ, Ctr Atmospher Chem Study, Dept Environm Sci & Engn, Shanghai 200433, Peoples R China
[2] Chinese Res Inst Environm Sci, Beijing 100012, Peoples R China
[3] China CDC, Inst Environm Hlth & Related Prod Safety, Beijing 100021, Peoples R China
[4] Univ Calif Davis, Dept Environm Toxicol, Davis, CA 95616 USA
[5] Univ Tennessee, Dept Civil & Environm Engn, Knoxville, TN 37996 USA
基金
中国国家自然科学基金;
关键词
Dust storm; Pollution; Mixing; Transformation; Long-range transport; AEROSOLS; EVENTS; SEASON;
D O I
10.1016/j.atmosenv.2010.06.011
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
To study the mixing and transformation of Asian dust with pollution in the two dust storms over the northern China in 2006, both TSP and PM2.5 samples were collected at three sites of northern China in addition to the dry deposition samples collected in an episode in Beijing. 23 elements, 15 ions, and 16 PAHs in each sample were analyzed. The two dust storms in northern China were observed in April 8-10 (DS1) and April 16-18 (DS2). Compared to DS2, DS1 was weaker and more polluted with stronger mixing between crustal and pollutant aerosols during their long-range transport. The concentrations of pollution species, e.g. pollution elements, ions, and PAHs were higher in DS1 than that in DS2, while the crustal species showed adverse variation. The correlation between chemical species and Al and between PAH(4) and PAH(5,6) further confirmed the stronger chemical transformation and aerosol mixing in DS1 than that in DS2. Back trajectory and chemical analysis revealed that in DS1 the air masses at Beijing were mostly from southern or southwestern direction at lower altitude with much more pollution, while in DS2 the air masses were mostly from the northwestern and northern direction with dust mainly, which explained why there was a stronger mixing of dust with pollution aerosol in DS1 than that in DS2 over Beijing. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3394 / 3403
页数:10
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