Formation Mechanisms for Secondary
Organic Aerosol in Ambient Air

Tadeusz Kleindienst1, Edward Edney1, Michael Lewandowski1, John Offenberg1, Mohammed Jaoui2, John Seinfeld3
1EPA Office of Research & Development; 2Alion Science and Technology; California Institute of Technology.

Abstract. An integrated laboratory and field research program is
underway at the National Exposure Research Laboratory to characterize
organic carbon in PM25 formed through chemical reactions. Information
from this study will provide critical data needed to improve the treatment
of secondary organic aerosol (SOA) formation in the Community
Multiscale Air Quality (CMAQ) model. In the laboratory portion, SOA-
producing hydrocarbon precursors are irradiated in a smog chamber in
the presence of NOx and S02. Identifiable organic compounds are
formed indicative of the precursors which are then compared to field
study samples to ensure that relevant chemical systems are being
studied. In collaboration with the California Institute of Technology and
the University of Antwerp, analytical methods and instruments are used
to identify the products. Collaborative efforts are also underway with the
Atmospheric Modeling Division of the NERL to incorporate findings from
the field and laboratory measurements to improve the treatment of SOA
within CMAQ. The project results should provide the Office of Air Quality
Planning and Standards with critical data on important regulatory issues,
among them (1) contributions of each SOA precursor to the PM25
concentration, (2) relative contributions of anthropogenic and biogenic
hydrocarbons to ambient SOA concentrations, and (3) impacts of S02
reductions on SOA formation. This information will improve the treatment
of SOA in the CMAQ model and help states evaluate control strategies
for reducing ambient PM25. These results will support effective
regulations and information that improves public health and reduces
ecological impacts.

Goals and Objectives

¦	Identify the major SOA precursors important in PM2.5

¦	Identify tracer compounds for the major SOA precursors

The figure below shows graphically the research approach
taken to conducts combined field and laboratory studies.

Schematic of Approach for Implementation Studies

Smog Chamber

(controlled simulation
of the atmosphere)

Real Atmosphere

hv

Out} "

amm sul

Outputs
SOA Tracers
Effects of Pollutants

Impacts

Exposure
assay

Sampling

hv



HC. NO*, so: L'miHlcHM
+ sanlight

t

Outcomes
Atmospheric Models

Experimental Methods

• Irradiate individual aromatic and biogenic hydrocarbons in the
presence of NOx and S02 in the NERL smog chamber and measure
their formation SOA masses.

Results and Conclusions

•	Smog chamber irradiations of biogenic hydrocarbons (emitted from
trees and other vegetation) and aromatic hydrocarbons (emitted
mainly from cars) show that these compound can be converted to
SOA by chemical reaction.

•	For compounds, such as isoprene and a-pinene, the addition of
S02 increases the amount of SOA formed above that obtained in its
absence.

•	Laboratory results suggest that several chemical processes must
be included in a mode! to explain SOA formation. The types of
processes that appear to be important include (1) exchange of
organic compounds between the gas and particle phases, often
referred to as partitioning, (2) acid catalyzed reactions within the
particle, (3) polymer formation, and possibly (4) cloud water
reactions could be contributing to SOA formation.

•	Toluene, a-pinene, and isoprene SOA tracer compounds detected
in ambient PM25 samples collected in the eastern USA indicate
these emitted hydrocarbons are contributing to SOA. Analysis of
field data suggests that SOA in the summer is significant, but
decreases considerably in the colder seasons.

•	The figure below shows how the concentrations of the tracer
compounds change with season. The isoprene tracer is only seen in
the summertime, while the tracer compound for a-pinene is detected
in the spring, summer, and fall. Levoglucosan, a primary product
from wood combustion, is detected throughout the year but mainly
during the winter and spring.

•	Determine reaction mechanisms for SOA formation

*	Work with the NERL Atmospheric Modeling Division (AMD) to
improve treatment of SOA in CMAQ.

•Use the NERL smog chamber to generate atmospherically
relevant air mixtures for exposure studies

The haze from Look Rock in the Great Smokey Mountains shows
the presence of secondary organic aerosol from photooxidation
reactions or ozone reactions with biogenic hydrocarbons.

	

Approach for Research Studies

1 Conduct field studies to measure the organic fraction of ambient

PM,

Identify tracer compounds in the ambient samples, such as

those that would be collected from the atmosphere depicted above.

•	Conduct laboratory experiments to identify reaction systems
responsible for the observed tracer compounds. Use the NERL
smog chamber to generate these atmospheres. Establish reaction
mechanisms for SOA formation.

•	Conduct modeling studies to predict the formation and partitioning
of SOA within PM2 5.

•	Collaborate with the Atmospheric Modeling Division (AMD) in
NERL to incorporate the findings in CMAQ.

•	Analyze chamber SOA samples using LC/MS, derivative-based
GC/'MS, Ion Trap MS, and MALDI methods to identify SOA tracer
compounds.

•	Compare chamber composition and concentration data with model
predictions whose formation mechanisms include contributions from
gas-aerosol partitioning, acid catalyzed reactions, and polymer
formation, and others.

•	Assess whether tracer concentrations can be used to determine
contributions of SOA precursors to ambient PM2 5.

Types of Experiments Conducted

2003 RTP PM2.5 Concentrations Data

Lab Irradiation Experiments

Field Studies

Toluene/NOx/SC>2

RTP, NC 2000 summer

a-Pinene/NOx /Air + S02

RTP, NC 2003

jS-Pinene/NOx/Air

Baltimore, MD 2001 summer

cMimonene/NOx/Air

Philadelphia, PA 2001 summer

lsoprene/NOx/Air + S02

New York City, NY 2001 summer

Toluene/a-Pinene/NOx + SO2

Detroit, Ml 2004 summer

a-Pinene/j3-Pinene/d-limonene/NOx



1 so pre ne/a-Pi nene/NOx



lsoprene/a-Pinene/Toluene/NOx + SO2



350

Isoprene
SOA Tracer

Nature of the Collaborations

•	The identification of individual polar organic compounds requires highly
specialized instruments and the skill to operate them and interpret the data.

•	The identification of tracer compounds requires gas chromatography to
measure individual compounds. We currently conduct these measurements
for samples taken in the United States. We are collaborating with researchers
at the University of Antwerp who are using similar techniques for samples
taken in Europe and South America.

•	We also have a collaboration with researchers at the California Institute of
Technology who are developing techniques using liquid chromatography and
mass spectroscopy to measure oligomeric and polymeric components of PM2 5

•	Physical scientists in the Human Exposure and Atmospheric Sciences
Division are collaborating with meteorologists in the Atmospheric Modeling
Division to incorporate the field and laboratory findings from this study into
CMAQ.

•We are working closely with NERL MCEAD in developing MALDI analysis
techniques to explore the potential of oligomer formation in the atmosphere.

150 20D 250

Julian Day 2003

Outputs, Outcomes and Future Directions

•	Continue comparing chamber concentrations and compositions of
SOA formed with atmospherically relevant individual and mixtures of
hydrocarbons irradiated in the presence of NOx and SO2 with model
results for proposed SOA formation mechanisms.

•	Assess whether SOA yields in complex hydrocarbon mixtures are
additive.

•	Work with AMD modelers to develop the CMAQ version of the PM
chemistry model. Results of the laboratory and field studies are
used by AMD in the CMAQ model that will be available to the RPOs
for State Implementation Plan modeling studies.

•	Results of the laboratory and field studies are used by AMD in the
CMAQ model that will be available to the RPOs for State
Implementation Plan modeling studies.

•	Some of the laboratory methods, developed under this program,
will be used in EPA-NOAA collaborative research to assess the
impact of N2O5 reactions on PM2.5 nitrate levels.

Disclaimer

Although this work was reviewed by EPA and approved for publication,
it may not necessarily reflect official Agency policy.



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