Size, composition, and mixing state of individual aerosol particles in a South China coastal city

被引:59
|
作者
Li, Weijun [1 ,2 ,4 ]
Shao, Longyi [1 ,2 ]
Wang, Zhishi [3 ]
Shen, Rongrong [1 ,2 ]
Yang, Shusheng [1 ,2 ]
Tang, Uwa [3 ]
机构
[1] China Univ Min & Technol Beijing, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China
[2] China Univ Min & Technol Beijing, Coll Geosci & Surveying Engn, Beijing 100083, Peoples R China
[3] Univ Macau, Fac Sci & Technol, Macau, Peoples R China
[4] Shandong Univ, Environm Res Inst, Jinan 250100, Shandong, Peoples R China
基金
中国博士后科学基金;
关键词
individual aerosol particles; soot; heterogeneous reaction; sea salt; POLYCYCLIC AROMATIC-HYDROCARBONS; AIRBORNE PARTICULATE MATTER; ATMOSPHERIC AEROSOLS; MAJOR ROADS; AIR; CLIMATE; NITRATE; MACAO; TRANSFORMATION; TRANSPORT;
D O I
10.1016/S1001-0742(09)60146-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Aerosol samples were collected in summer in Macao, a coastal city of the Pearl River Delta Region in China. Morphology, size, elemental composition, and mixing state of individual aerosol particles were determined by scanning electron microscopy coupled energy dispersive X-ray (SEM/EDX) and transmission electron microscopy (TEM). Based on the morphologies of 5711 aerosol particles, they consist of soot (32%), mineral (17%), secondary. (22%), and unknown fine particles (29%). The sizes of these particles were mostly distributed between 0.1 and 0.4 mu m. Compositions of 202 mineral particles were obtained by SEM/EDX. Mineral particles were mainly classified into three types: Si-rich, Ca-rich, and Na-rich. The compositions of typical mineral particles can indicate their sources in sampling location. For example, mineral particles, collected along the main street, were associated with trace amounts of heavy metals, such as Zn, Ti, Mn, Ba, Pb, and As. TEM observations indicate that most Na-rich particles were aged sea salt particles (e.g., Na2SO4 and NaNO3) which formed through heterogeneous chemical reactions between sea salt and acidic gases. Additionally, aging time of soot was short in Macao due to high humidity, high temperature, and high levels of sunlight in Macao. Most of soot and fine mineral dust particles were internally mixed with secondary particles.
引用
收藏
页码:561 / 569
页数:9
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