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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 108, NO. D2,
4041,
doi:10.1029/2001JD000797,
2003
Speciation of volatile organic compound emissions for regional air quality modeling of particulate matter and ozone
P. A. Makar
Modelling and Integration Division, Air Quality Research Branch,
Meteorological Service of Canada,
Toronto,
Ontario,
Canada
M. D. Moran
Modelling and Integration Division, Air Quality Research Branch,
Meteorological Service of Canada,
Toronto,
Ontario,
Canada
M. T. Scholtz
Canadian Ortech Environmental, Inc.,
Mississauga,
Ontario,
Canada
A. Taylor
Canadian Ortech Environmental, Inc.,
Mississauga,
Ontario,
Canada
Abstract
A new classification scheme for the speciation of organic compound emissions for use in air quality models is described. The
scheme uses 81 organic compound classes to preserve both net gas-phase reactivity and particulate matter (PM) formation potential.
Chemical structure, vapor pressure, hydroxyl radical (OH) reactivity, freezing point/boiling point, and solubility data were
used to create the 81 compound classes. Volatile, semivolatile, and nonvolatile organic compounds are included. The new classification
scheme has been used in conjunction with the Canadian Emissions Processing System (CEPS) to process 1990 gas-phase and particle-phase
organic compound emissions data for summer and winter conditions for a domain covering much of eastern North America. A simple
postprocessing model was used to analyze the speciated organic emissions in terms of both gas-phase reactivity and potential
to form organic PM. Previously unresolved compound classes that may have a significant impact on ozone formation include biogenic
high-reactivity esters and internal C6–8 alkene-alcohols and anthropogenic ethanol and propanol. Organic radical production associated with anthropogenic organic
compound emissions may be 1 or more orders of magnitude more important than biogenic-associated production in northern United
States and Canadian cities, and a factor of 3 more important in southern U.S. cities. Previously unresolved organic compound
classes such as low vapour pressure PAHs, anthropogenic diacids, dialkyl phthalates, and high carbon number alkanes may have
a significant impact on organic particle formation. Primary organic particles (poorly characterized in national emissions
databases) dominate total organic particle concentrations, followed by secondary formation and primary gas-particle partitioning.
The influence of the assumed initial aerosol water concentration on subsequent thermodynamic calculations suggests that hydrophobic
and hydrophilic compounds may form external mixtures, and that separate treatment for these groups may be required in future
air quality model simulations. The post-processing model used here overestimates the organic particle formation relative to
measurements, lacks the complexity of a regional air quality model, and is not intended as an alternative to the latter. Results
from the post-processing model do, however, provide guidance for the treatment of organic gases and particles in future air
quality modeling work. Future air quality model simulations should attempt to speciate primary particulate organic compounds
and include more detailed organic compound classes. Future emissions profile measurements should speciate gaseous high-molecular-mass
organic compounds and primary organics emitted in particulate form (primary particle emissions are only available as a total
particulate mass in currently available emissions data).
Published 16
January
2003.
Index Terms: 0322 Atmospheric Composition and Structure: Constituent sources and sinks; 0305 Atmospheric Composition and Structure: Aerosols and particles (0345, 4801); 0365 Atmospheric Composition and Structure: Troposphere—composition and chemistry.
Read Full Article (file size: 5317486 bytes) Cited by
Citation: Makar, P. A., M. D. Moran, M. T. Scholtz, and A. Taylor
(2003),
Speciation of volatile organic compound emissions for regional air quality modeling of particulate matter and ozone,
J. Geophys. Res.,
108(D2),
4041,
doi:10.1029/2001JD000797.
Published in 2003 by the American Geophysical Union.
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