Chemical composition of urban airborne particulate matter in Ulaanbaatar

被引:29
|
作者
Nishikawa, Masataka [1 ]
Matsui, Ichiro [1 ]
Batdorj, Dashdondog [2 ]
Jugder, Dulam [2 ]
Mori, Ikuko [1 ]
Shimizu, Atsushi [1 ]
Sugimoto, Nobuo [1 ]
Takahashi, Katsuyuki [1 ]
机构
[1] Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan
[2] Natl Agcy Meteorol & Environm Monitoring, Inst Meteorol & Hydrol, Ulaanbaatar 210646 46, Mongolia
关键词
Ulaanbaatar; Urban airborne particulate matter; Chemical composition; Stable carbon isotope ratio; Coal; Soil dust; AEROSOLS; CARBON;
D O I
10.1016/j.atmosenv.2011.07.029
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Atmospheric pollution caused by airborne particulate matter in the winter season in Ulaanbaatar, Mongolia is a very serious problem. However, there is a complete lack of scientific observation data to define the situation prior to any remediation. PM10 and PM2.5 average monthly values obtained by continuous monitoring showed the concentrations of particles of both size categories exceeded 100 mu g m(-3) during November to February (winter). PM10 particles were sampled with filters in January (i.e. during the heating period) and June (i.e.non-heating period) of 2008 in central Ulaanbaatar. To determine the composition of urban airborne particulate matter we analyzed a range of ionic components, multiple elements including heavy metals, and organic and inorganic carbon (soot). We also measured the stable carbon isotope ratio of the soot. Total carbon (sum of organic carbon and inorganic carbon) accounted for 47% of the mass of the PM10 during the heating period and 33% during the non-heating period, and was the largest component of urban airborne particulate matter in Ulaanbaatar. Stable isotope ratios (delta C-13) of soot generated during the heating period (-23.4 +/- 0.2 parts per thousand) approximated the ratios for coal used in Ulaanbaatar (-21.3 to -24.4 parts per thousand), while the ratios during the non-heating period (-27.1 +/- 0.4 parts per thousand) were clearly different from the coal values. In the heating period, a very high correlation was observed between soot and organic carbon, SO42-, NO3-, F-, Zn, As, and Pb, and we concluded that they were derived from coal combustion along with soot. In addition, the concentrations and their ratios relative to each other of Al, Fe, Ca, K, Na, Mg, and Mn hardly differed between the heating period and the non-heating period, and it was concluded that they were derived from soil dust. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:5710 / 5715
页数:6
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