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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 110,
D16305,
doi:10.1029/2004JD005623,
2005
Budget of organic carbon in a polluted atmosphere: Results from the New England Air Quality Study in 2002
J. A. de Gouw
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
A. M. Middlebrook
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
C. Warneke
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
P. D. Goldan
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
W. C. Kuster
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
J. M. Roberts
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
F. C. Fehsenfeld
Aeronomy Laboratory, NOAA, Boulder, Colorado, USA
D. R. Worsnop
Aerodyne Research Inc., Billerica, Massachusetts, USA
M. R. Canagaratna
Aerodyne Research Inc., Billerica, Massachusetts, USA
A. A. P. Pszenny
Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, New Hampshire, USA
W. C. Keene
Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia, USA
M. Marchewka
Department of Chemistry, Western Michigan University, Kalamazoo, Michigan, USA
S. B. Bertman
Department of Chemistry, Western Michigan University, Kalamazoo, Michigan, USA
T. S. Bates
Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA
Abstract
An extensive set of volatile organic compounds (VOCs) and particulate organic matter (POM) was measured in polluted air during
the New England Air Quality Study in 2002. Using VOC ratios, the photochemical age of the sampled air masses was estimated.
This approach was validated (1) by comparing the observed rates at which VOCs were removed from the atmosphere with the rates
expected from OH oxidation, (2) by comparing the VOC emission ratios inferred from the data with the average composition of
urban air, and (3) by the ability to describe the increase of an alkyl nitrate with time in terms of the chemical kinetics.
A large part of the variability observed for oxygenated VOCs (OVOCs) and POM could be explained by a description that includes
the removal of the primary anthropogenic emissions, the formation and removal of secondary anthropogenic species, and a biogenic
contribution parameterized by the emissions of isoprene. The OVOC sources determined from the data are compared with the available
literature, and a satisfactory agreement is obtained. The observed sub-μm POM was highly correlated with secondary anthropogenic
gas-phase species, strongly suggesting that the POM was from secondary anthropogenic sources. The results are used to describe
the speciation and total mass of gas- and particle-phase organic carbon as a function of the photochemical age of an urban
air mass. Shortly after emission the organic carbon mass is dominated by primary VOCs, while after two days the dominant contribution
is from OVOCs and sub-μm POM. The total measured organic carbon mass decreased by about 40% over the course of two days. The
increase in sub-μm POM could not be explained by the removal of aromatic precursors alone, suggesting that other species must
have contributed and/or that the mechanism for POM formation is more efficient than previously assumed.
Received 22
November
2004;
accepted 14
June
2005;
published 30
August
2005.
Keywords: volatile organic compounds;
particulate organic matter;
polluted atmosphere.
Index Terms: 0345 Atmospheric Composition and Structure: Pollution: urban and regional (0305, 0478, 4251); 0355 Atmospheric Composition and Structure: Thermosphere: composition and chemistry; 0322 Atmospheric Composition and Structure: Constituent sources and sinks; 0315 Atmospheric Composition and Structure: Biosphere/atmosphere interactions (0426, 1610); 0305 Atmospheric Composition and Structure: Aerosols and particles (0345, 4801, 4906).
Read Full Article (file size: 2729996 bytes) Cited by
Citation: de Gouw, J. A., et al.
(2005),
Budget of organic carbon in a polluted atmosphere: Results from the New England Air Quality Study in 2002,
J. Geophys. Res.,
110,
D16305,
doi:10.1029/2004JD005623.
Copyright 2005 by the American Geophysical Union.
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