Molecular markers of biomass burning, fungal spores and biogenic SOA in the Taklimakan desert aerosols

被引:57
作者
Fu, Pingqing [1 ,7 ]
Zhuang, Guoshun [2 ]
Sun, Yele [1 ]
Wang, Qiongzhen [2 ,5 ]
Chen, Jing [4 ]
Ren, Lujie [1 ]
Yang, Fan [1 ]
Wang, Zifa [1 ]
Pan, Xiaole [6 ]
Li, Xiangdong [7 ]
Kawamura, Kimitaka [3 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, LAPC, Beijing 100029, Peoples R China
[2] Fudan Univ, Dept Environm Sci & Engn, Ctr Atmospher Chem Study, Shanghai 200433, Peoples R China
[3] Hokkaido Univ, Inst Low Temp Sci, Sapporo, Hokkaido 0600819, Japan
[4] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
[5] Zhejiang Environm Sci & Design Inst, Hangzhou 310007, Zhejiang, Peoples R China
[6] Kyushu Univ, Appl Mech Res Inst, Fukuoka 812, Japan
[7] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Kowloon, Hong Kong, Peoples R China
基金
日本学术振兴会;
关键词
Biomass burning; Fungal spore; 2-Methyltetrols; Asian dust; Taklimakan desert; SECONDARY ORGANIC AEROSOL; WESTERN NORTH PACIFIC; ASIAN DUST; ATMOSPHERIC AEROSOLS; EMISSION FACTORS; CHEMICAL-COMPOSITION; PARTICULATE MATTER; MARINE AEROSOLS; TRACERS; POLLUTION;
D O I
10.1016/j.atmosenv.2015.10.087
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Biogenic primary organic aerosols (POA) and secondary organic aerosols (SOA) are important organic constituents of atmospheric particulate matter (PM). In order to better understand the atmospheric abundances, molecular compositions and sources of the desert aerosols, biomass-burning tracers (e.g. levoglucosan), primary saccharides including fungal spore tracers, and SOA tracers from the oxidation of biogenic volatile organic compounds (e.g. isoprene, monoterpenes and sesquiterpene) have been studied in ambient aerosols from the Taklimakan desert, using gas chromatography-mass spectrometry. Results showed that the total concentrations of biomass-burning tracers at Hetian (177-359 ng m(-3), mean 233 ng m(-3) in PM2.5) in the south rim of the desert were much higher than those at Tazhong (1.9-8.8 ng m(-3) in PM2.5 and 5.9-32 ng m(-3) in TSP) in the central Taklimakan desert. Molecular markers of fungal spores were also detected in all the desert aerosols, highlighting the importance of primary bioaerosols in the Asian dust particles. A specific pattern of the dominance of 2-methylglyceric acid over 2-methyltetrols and C-5-alkene triols was found in the Taklimakan desert aerosols, especially during the dust storm events, which is different from the 2-methyltetrols-dominated pattern in other ambient aerosols. Our results provide direct evidence on the biogenic POA and SOA tracers in the Taklimakan desert region, which help to better understand their impact on the aerosol chemistry in the down-wind regions. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:64 / 73
页数:10
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