Single particle mass spectrometry of oxalic acid in ambient aerosols in Shanghai: Mixing state and formation mechanism

被引:93
|
作者
Yang, Fan [1 ]
Chen, Hong [1 ]
Wang, Xinning [1 ]
Yang, Xin [1 ]
Du, Jianfei [1 ,2 ]
Chen, Jianmin [1 ]
机构
[1] Fudan Univ, Dept Environm Sci & Engn, Shanghai 200433, Peoples R China
[2] Shanghai Baoshan Meteorol Stn, Shanghai 201901, Peoples R China
基金
中国国家自然科学基金;
关键词
Oxalic acid; ATOFMS; Mixing state; Formation mechanism; DICARBOXYLIC-ACIDS; CHEMICAL-CHARACTERIZATION; ATMOSPHERIC PARTICLES; ISOTOPIC COMPOSITIONS; INDIVIDUAL PARTICLES; SIZE DISTRIBUTIONS; REAL-TIME; CHEMISTRY; EMISSIONS; CLOUD;
D O I
10.1016/j.atmosenv.2009.05.002
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Oxalic acid in individual aerosol particles was measured using single particle aerosol time-of-flight mass spectrometry (ATOFMS) in the summer of 2007 in Shanghai, China. Oxalate was found in 3.4% of total particles with diameters in the range of 0.2 - 2.0 mu m. Size, chemical composition and hourly temporal counts of single particles that contained oxalic acid were measured. The predominant types of oxalate-containing particles were characterized to distinguish the primary and secondary sources of oxalic acid. Biomass burning was revealed as a major primary source of oxalic acid which contributed more than 20% of the oxalate-containing particles. Evidences for two different formation pathways of oxalic acid were observed in our experiment. The number fraction of oxalate-containing particles correlated with that of sulfate particles and the changes of air parcel backward trajectories, suggesting that in-cloud processing played important roles in oxalic acid formation. The diurnal patterns of dust and sea salt particle counts fitted well with the ambient relative humidity variation, suggesting that heterogeneous reactions occurring in hydrated/deliquesced aerosols also contributed to the production of oxalic acid. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3876 / 3882
页数:7
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