Characterization of polar organic components in fine aerosols in the southeastern United States: Identity, origin, and evolution

被引:113
作者
Gao, Song
Surratt, Jason D.
Knipping, Eladio M.
Edgerton, Eric S.
Shahgholi, Mona
Seinfeld, John H.
机构
[1] CALTECH, Dept Environm Sci & Engn, Pasadena, CA 91125 USA
[2] CALTECH, Dept Chem Engn, Pasadena, CA 91125 USA
[3] CALTECH, Dept Chem, Pasadena, CA 91125 USA
[4] Elect Power Res Inst, Palo Alto, CA 94304 USA
[5] Atmospher Res & Anal Inc, Cary, NC 27513 USA
关键词
D O I
10.1029/2005JD006601
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Filter samples of fine aerosols collected in the Southeastern United States in June 2004 were analyzed for the characterization of polar organic components. Four analytical techniques, liquid chromatography-mass spectrometry, ion trap mass spectrometry, laser desorption ionization mass spectrometry, and high-resolution mass spectrometry, were used for identification and quantification. Forty distinct species were detected, comprising on average 7.2% and 1.1% of the total particulate organic mass at three inland sites and a coastal site, respectively. The relative abundance of these species displays a rather consistent distribution pattern in the inland region, whereas a different pattern is found at the coastal site. Chemical and correlation analyses suggest that the detected species are secondary in nature and originate from terpene oxidation, with possible participation of NOx and SO2. It is estimated that polar, acidic components in fine aerosols in the Southeastern United States cover a molecular weight range of 150-400 Da and do not appear to be oligomeric. Other components with MW up to 800 Da may also be present. The detected polar organic species are similar to humic-like substances (HULIS) commonly found in fine aerosols in other rural areas. We present the first, direct evidence that atmospheric processing of biogenic emissions can lead to the formation of certain HULIS species in fine aerosols, and that this may be a typical pathway in the background atmosphere in continental regions; nevertheless, a natural source for HULIS, such as from aquatic and/or terrestrial humic/fulvic acids and their degradation products, cannot be precluded.
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