TY - JOUR
T1 - Organic molecular compositions and size distributions of Chinese summer and autumn aerosols from Nanjing
T2 - Characteristic haze event caused by wheat straw burning
AU - Wang, Gehui
AU - Kakawamura, Kimita
AU - Xie, Mingjie
AU - Hu, Shuyuan
AU - Cao, Junji
AU - An, Zhisheng
AU - Waston, John G.
AU - Chow, Judith C.
PY - 2009/9/1
Y1 - 2009/9/1
N2 - Size-segregated aerosol samples were collected in urban Nanjing, China during summer and autumn of 2007 including a period of hazy days during June 1-5. Organic aerosols in the haze event were characterized by elevated concentrations of levoglucosan, high molecular weight (HMW) n-alkanes, and HMW fatty acids due to the emissions from field burning of wheat straw. In contrast, organic aerosols on nonhazy days were characterized by a predominance of fossil fuel combustion products. Levoglucosan (4030 ng m-3), n-alkanes (1520 ng m-3), fatty acids (2629 ng m-3), and PAHs (57 ng m-3) in the haze samples were 3-40 times more abundant than those innoneventsamples. Approximately 30-90%of the organics during the haze period can be attributed to wheat straw burning. Concentrations of particulate material (PM) mass, n-alkanes, and low molecular weight (LMW) PAHs showed a unimodal size distribution, peaking at 0.7-1.1 μm during the hazy days, and a bimodal distribution, peaking at 0.7-1.1 μm and 4.7-5.8 μm during nonhazy days. The geometric mean diameters (GMDs) of organic aerosols are larger in the fine mode(<2.1μm)during the hazy days, suggesting aerosols emitted from the wheat straw burning are larger than those from fossil fuel combustion, and fine particle coagulation and organic compound repartitioning were enhanced.
AB - Size-segregated aerosol samples were collected in urban Nanjing, China during summer and autumn of 2007 including a period of hazy days during June 1-5. Organic aerosols in the haze event were characterized by elevated concentrations of levoglucosan, high molecular weight (HMW) n-alkanes, and HMW fatty acids due to the emissions from field burning of wheat straw. In contrast, organic aerosols on nonhazy days were characterized by a predominance of fossil fuel combustion products. Levoglucosan (4030 ng m-3), n-alkanes (1520 ng m-3), fatty acids (2629 ng m-3), and PAHs (57 ng m-3) in the haze samples were 3-40 times more abundant than those innoneventsamples. Approximately 30-90%of the organics during the haze period can be attributed to wheat straw burning. Concentrations of particulate material (PM) mass, n-alkanes, and low molecular weight (LMW) PAHs showed a unimodal size distribution, peaking at 0.7-1.1 μm during the hazy days, and a bimodal distribution, peaking at 0.7-1.1 μm and 4.7-5.8 μm during nonhazy days. The geometric mean diameters (GMDs) of organic aerosols are larger in the fine mode(<2.1μm)during the hazy days, suggesting aerosols emitted from the wheat straw burning are larger than those from fossil fuel combustion, and fine particle coagulation and organic compound repartitioning were enhanced.
UR - https://www.scopus.com/pages/publications/69549083458
U2 - 10.1021/es803086g
DO - 10.1021/es803086g
M3 - 文章
C2 - 19764207
AN - SCOPUS:69549083458
SN - 0013-936X
VL - 43
SP - 6493
EP - 6499
JO - Environmental Science and Technology
JF - Environmental Science and Technology
IS - 17
ER -