Chemical Characteristics of Carbonaceous Aerosols During Dust Storms over Xi'an in China

被引:9
|
作者
Li Xuxiang [1 ]
Cao Junji [1 ,2 ]
Chow, Judith [3 ]
Han Yongming [2 ]
Lee, Shuncheng [4 ]
Watson, John [3 ]
机构
[1] Xi An Jiao Tong Univ, Dept Environm Sci & Technol, Xian 710049, Peoples R China
[2] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
[3] Univ Nevada, Desert Res Inst, Reno, NV 89506 USA
[4] Hong Kong Polytech Univ, Hong Kong, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
carbonate carbon; organic carbon; elemental carbon; dust storm;
D O I
10.1007/s00376-008-0847-1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Characterization of carbonaceous aerosols including CC (carbonate carbon), OC (organic carbon), and EC (elemental carbon) were investigated at Xi'an, China, near Asian dust source regions in spring 2002. OC varied between 8.2 and 63.7 mu g m(-3), while EC ranged between 2.4 and 17.2 mu m(-3) during the observation period. OC variations followed a similar pattern to EC and the correlation coefficient between CC and EC is 0.89 (n=31). The average percentage of total carbon (TC, sum of CC, CC, and EC) in PM2.5 during dust storm (DS) events was 13.6%, which is lower than that during non-dust storm (NDS) periods (22.7%). CC, CC, and EC accounted for 12.9%, 70.7%, and 16.4% of TC during DS events, respectively. The average ratio of OC/EC was 5.0 in DS events and 3.3 in NDS periods. The OC-EC correlation (R-2=0.76, n=6) was good in DS events, while it was stronger (R-2=0.90, n=25) in NDS periods. The percentage of water-soluble OC (WSOC) in TC accounted for 15.7%, and varied between 13.3% and 22.3% during DS events. The distribution of eight carbon fractions indicated that local emissions such as motor vehicle exhaust were the dominant contributors to carbonaceous particles. During DS events, soil dust dominated the chemical composition, contributing 69% to the PM2.5 mass, followed by organic matter (12.8%), sulfate (4%), EC (2.2%), and chloride (1.6%). Consequently, CC was mainly entrained by Asian dust. However, even in the atmosphere near Asian dust source regions, OC and EC in atmospheric dust were controlled by local emission rather than the transport of Asian dust.
引用
收藏
页码:847 / 855
页数:9
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