The evolution of chemical components of aerosols at five monitoring sites of China during dust storms

被引:92
作者
Wang, Ying
Zhuang, Guoshun [1 ]
Tang, Aohan
Zhang, Wenjie
Sun, Yele
Wang, Zifa
An, Zhisheng
机构
[1] Fudan Univ, Ctr Atmospher Chem Study, Dept Environm Sci & Engn, Shanghai 200433, Peoples R China
[2] Beijing Normal Univ, Dept Chem, Ctr Atmospher Environm Study, Beijing 100875, Peoples R China
[3] Chinese Acad Sci, NZC, LAPC, Inst Atmospher Phys, Beijing 100029, Peoples R China
[4] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
基金
中国国家自然科学基金;
关键词
dust storm; evolution; source contribution; PM2.5; TSP;
D O I
10.1016/j.atmosenv.2006.09.015
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Daily PM2.5 and TSP and their chemical composition with two dust events (DSI: 9-10 March and DS2: 27-30 March) were simultaneously observed for the period of 9 March-23 April 2004 from a monitoring network over China. Five monitoring sites were performed along the transport pathway of Asian dust storm, located in Northwest, North, East, and Southeast regions of China. The dust and non-dust days exhibited different characteristics with respect to the composition and the meteorological conditions. In non-dust days, particulate pollution was found to be associated with the city economy, and it primarily consisted of the crustal, the secondary, and the carbonaceous material. In the dust episodes, significant increase in the particle concentration with a large part of the secondary components diluted by the crustal components was observed at all the sites. Particles were getting more and more acidic as the episodic dust progressed eastward. Dust particles were suggested to react with S02/NOx/sulfate/nitrate based on the variations of So(4)(2-)/Ca2+ and No-3(-)/Ca-2(+) along the transport pathway, and the formation mechanism of sulfate and nitrate was proved to be different. Positive matrix factorization analysis showed that the sources from the upstream and the transport pathways could account for 49%, 82%, and 28% of PM mass, crust, and secondary aerosol, respectively, and the contribution decreased, as the dust made its way from source area to the coastal regions. Enrichment factors of the species presented significant correlations among different sites in the dust episodes, suggesting the significant impact of those dust emissions on the local environment. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1091 / 1106
页数:16
相关论文
共 41 条
[1]   Eolian factor in the process of modern salt accumulation in western Dzungaria, China [J].
Abuduwaili, Jilili ;
Mu Guijin .
EURASIAN SOIL SCIENCE, 2006, 39 (04) :367-376
[2]  
[Anonymous], 2019, THE J, DOI DOI 10.1590/0103-6440201902280
[3]   Mass-particle size distributions of atmospheric dust and the dry deposition of dust to the remote ocean [J].
Arimoto, R ;
Ray, BJ ;
Lewis, NF ;
Tomza, U ;
Duce, RA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D13) :15867-15874
[4]   Elemental composition and sources of air pollution in the city of Chandigarh, India, using EDXRF and PIXE techniques [J].
Bandhu, HK ;
Puri, S ;
Garg, ML ;
Singh, B ;
Shahi, JS ;
Mehta, D ;
Swietlicki, E ;
Dhawan, DK ;
Mangal, PC ;
Singh, N .
NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS, 2000, 160 (01) :126-138
[5]   Characterisation of chemical species in PM2.5 and PM10 aerosols in Brisbane, Australia [J].
Chan, YC ;
Simpson, RW ;
Mctainsh, GH ;
Vowles, PD ;
Cohen, DD ;
Bailey, GM .
ATMOSPHERIC ENVIRONMENT, 1997, 31 (22) :3773-3785
[6]   Characteristics of particles sampled in southern Taiwan during the Asian dust storm periods in 2000 and 2001 [J].
Chen, SJ ;
Hsieh, LT ;
Kao, MJ ;
Lin, WY ;
Huang, KL ;
Lin, CC .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (35) :5925-5934
[7]   The characteristics of carbonaceous species and their sources in PM2.5 in Beijing [J].
Dan, M ;
Zhuang, GS ;
Li, XX ;
Tao, HR ;
Zhuang, YH .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (21) :3443-3452
[8]   Role of mineral aerosol as a reactive surface in the global troposphere [J].
Dentener, FJ ;
Carmichael, GR ;
Zhang, Y ;
Lelieveld, J ;
Crutzen, PJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D17) :22869-22889
[9]   THE ATMOSPHERIC INPUT OF TRACE SPECIES TO THE WORLD OCEAN [J].
Duce, R. ;
Liss, P. ;
Merrill, J. ;
Atlas, E. ;
Buat-Menard, P. ;
Hicks, B. ;
Miller, J. ;
Prospero, J. ;
Arimoto, R. ;
Church, T. ;
Ellis, W. ;
Galloway, J. ;
Hansen, L. ;
Jickells, T. ;
Knap, A. ;
Reinhardt, K. ;
Schneider, B. ;
Soudine, A. ;
Tokos, J. ;
Tsunogai, S. ;
Wollast, R. ;
Zhou, M. .
GLOBAL BIOGEOCHEMICAL CYCLES, 1991, 5 (03) :193-259
[10]   Mineral particles collected in China and Japan during the same Asian dust-storm event [J].
Fan, XB ;
Okada, K ;
Niimura, N ;
Kai, K ;
Arao, K ;
Shi, GY ;
Qin, Y ;
Mitsuta, Y .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (02) :347-351