Correlation of secondary organic aerosol with odd oxygen in Mexico City

被引:145
作者
Herndon, Scott C. [1 ]
Onasch, Timothy B. [1 ]
Wood, Ezra C. [1 ]
Kroll, Jesse H. [1 ]
Canagaratna, Manjula R. [1 ]
Jayne, John T. [1 ]
Zavala, Miguel A. [5 ,7 ]
Knighton, W. Berk [4 ]
Mazzoleni, Claudio [8 ]
Dubey, Manvendra K. [8 ]
Ulbrich, Ingrid M. [9 ]
Jimenez, Jose L. [9 ]
Seila, Robert [6 ]
de Gouw, Joost A. [3 ]
de Foy, Benjamin [2 ]
Fast, Jerome [10 ]
Molina, Luisa T. [5 ,7 ]
Kolb, Charles E. [1 ]
Worsnop, Douglas R. [1 ]
机构
[1] Aerodyne Res Inc, Billerica, MA 01821 USA
[2] St Louis Univ, Dept Earth & Atmospher Sci, St Louis, MO 63103 USA
[3] NOAA, Earth Syst Res Lab, Boulder, CO 80305 USA
[4] Montana State Univ, Dept Chem & Biochem, Bozeman, MT 59717 USA
[5] Molina Ctr Energy & Environm, La Jolla, CA 92037 USA
[6] Natl Exposure Res Lab, Environm Protect Agcy, Res Triangle Pk, NC 27711 USA
[7] MIT, Cambridge, MA 02139 USA
[8] Los Alamos Natl Lab, Div Earth & Environm Sci, Los Alamos, NM 87545 USA
[9] Univ Colorado, Dept Chem & Biochem, Boulder, CO 80309 USA
[10] Pacific NW Natl Lab, Richland, WA 99352 USA
关键词
D O I
10.1029/2008GL034058
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Photochemically processed urban emissions were characterized at a mountain top location, free from local sources, within the Mexico City Metropolitan Area. Analysis of the Mexico City emission plume demonstrates a strong correlation between secondary organic aerosol and odd oxygen (O-3 + NO2). The measured oxygenated-organic aerosol correlates with odd oxygen measurements with an apparent slope of (104-180) mu g m(-3) ppmv(-1) (STP) and r(2) > 0.9. The dependence of the observed proportionality on the gas-phase hydrocarbon profile is discussed. The observationally-based correlation between oxygenated organic aerosol mass and odd oxygen may provide insight into poorly understood secondary organic aerosol production mechanisms by leveraging knowledge of gas-phase ozone production chemistry. These results suggest that global and regional models may be able to use the observed proportionality to estimate SOA as a co-product of modeled O-3 production until more complete models of SOA formation become available.
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