Collett Research Group Current Projects
Atmospheric Chemistry/Air Quality Program
Atmospheric Science Department
Colorado State University
Fort Collins, Colorado USA
Investigation of San Joaquin Valley
Fog Chemistry and Physics during the California Regional Particulate Air
Quality Study (CRPAQS)
Sponsor: San Joaquin Valleywide Air Pollution Study Agency
Project Period: September 2000 - August 2003
As part of the California Regional Particulate Air Quality Study (CRPAQS),
measurements of fog chemistry and physics are planned in the San Joaquin Valley
(SJV) of California. The primary objectives of the proposed fog study
are to:
- Provide a data set suitable for evaluating predictions of fog chemistry
and physics made as part of future numerical simulations of CRAPQS fog episodes.
Several specific items related to this objective are mentioned in subsequent
points.
- Measure spatial and temporal variations in ground-level SJV fog composition
during the CRPAQS winter intensive. These measurements will provide
an overview of CRPAQS fog composition and the potential for particle processing
by SJV fogs and will provide an important basis for evaluating numerical model
predictions. Measurements are planned at four locations. Three
of these locations will use new, automated fog sampling systems developed
for this study.
- Characterize vertical profiles of fog composition and liquid water
content for use in testing fog models and in developing a better understanding
of deposition processes and aerosol processing.
- Characterize the drop size-dependence of key fog solutes and the resulting
impact on solute deposition fluxes. These measurements will also be
key to validating future numerical simulations of CRPAQS fog episodes made
using a size-resolved fog chemistry model.
- Measure rates of inorganic (especially nitrate, sulfate and ammonium)
fog solute deposition during extended fog episodes in order to determine
the impact SJV fogs exert on boundary layer inorganic aerosol particle mass
concentrations. These measurements will also be used to constrain future
numerical simulations of particle processing by fogs and to examine how fog-related
solute removal fluxes vary with fog episode duration.
- Characterize the extent of carbonaceous particle processing by SJV
fogs and the importance of fog processing as a vector for removal of these
particles from the boundary layer.
- Examine the capacity of the atmosphere for new aerosol mass formation,
via aqueous S(IV) oxidation, during CRPAQS fog episodes. Such information
is a key component for understanding net effects of the fog episodes on boundary
layer sulfate concentrations.
The Organic Composition of Fogs
and Clouds
Sponsor: National Science Foundation
Project Period: August 2002 - July 2006
Studies conducted over the last two decades have clearly demonstrated
the important roles clouds and fogs play as processors of inorganic fine
aerosol particles, contributing both to production of new particle mass and
particle removal. Despite this progress, little is yet known about
interactions of fogs and clouds with carbonaceous aerosol particles and organic
trace gases. While several studies have found high organic solute concentrations
in both clouds and fogs, the composition and sources of that organic matter
are largely unknown. Previous investigations have typically identified
less than 30% of the dissolved organic content of collected cloud and fog
samples.
This project is designed to significantly increase knowledge of the organic
composition of clouds and fogs and the efficiency with which clouds and fogs
scavenge carbonaceous aerosol particles. The project includes a laboratory
development effort to improve capabilities for measuring concentrations of
the diverse organic species suspected to be present in cloud and fog drops
and a series of field experiments to collect samples suitable for application
of the developed suite of organic analytical techniques. The field
campaigns will be used to collect samples of cloud/fog types that are seasonally
important in three distinct environments: winter radiation fogs in the California’s
Central Valley, spring stratus clouds intercepting the coastal hills of Southern
California, and summer orographic clouds intercepting the western slope of
the Rocky Mountains. The first two campaigns will provide information
about the organic composition of fogs and clouds in two different urban environments
while the third study will gather information about the composition of clouds
at a less impacted continental site. The goal of the analytical work
is to significantly increase the fraction of fog/cloud organic matter that
is identified as specific organic compounds or characterized with respect
to its molecular weight and chemical properties. Additional field measurements
will reveal the efficiency of carbonaceous aerosol particle scavenging by
clouds and fogs and how this efficiency varies with particle source type.
Completion of this project is expected to yield several benefits. First,
a suite of analytical approaches suitable for characterization of organic
matter present in clouds and fogs will be developed, documented, and shared
with the atmospheric chemistry community. Second, information will
be gained about the total concentrations of organic matter present in three
important cloud types/environments while the composition of that organic
matter will be much better characterized than previously possible.
Increased information about the composition of organic material present in
fog and cloud drops will lend new insight into the ways that clouds and fogs
process carbonaceous aerosol particles and organic trace gases. Third,
field measurements of the scavenging efficiency of carbonaceous aerosol particles
by radiation fogs and stratus clouds will provide key information for inclusion
in air quality models. These findings will also provide new insight
into the potential influence of carbonaceous aerosol particles on earth’s
climate through modification of cloud properties (the indirect aerosol climate
effect). Last, the project will produce a number of broader impacts
including increasing the participation of women in the male-dominated field
of atmospheric science (the project will support training of two female atmospheric
scientists -one PhD student and one postdoctoral scientist), advancing discovery
and understanding while promoting teaching and learning (project results
will be incorporated into educational materials to be shared with students
and the community at a range of educational levels), and providing new information
helpful to making effective policy decisions in the areas of regional air
quality and climate change.
Field Investigation of Smoke
Plumes: aerosol Characterization and Testing of IMPROVE Assumptions
Sponsor: National Park Service
Project Period: September 2001 - August 2003
A summer 2002 field study in Yosemite National Park focused on the role
of smoke aerosol in regional haze. Field measurements included a suite
of physical and chemical measurements. These included characterizing
the complete aerosol size distribution, size-resolved chemical composition,
hygroscopic growth, and optical properties. Chemical measurements
included both time-integrated and semi-continuous measurements.
Review and interpretation of aerosol size distribution and hygroscopicity
data is currently underway. These data will be compared with other
project data sets, including aerosol composition measurements and measurements
of aerosol optical properties. A variety of measurements were made
during the Yosemite study to examine the ionic composition of regional aerosol.
These include collection of particulate matter with aerodynamic diameter
less than 2.5 micrometers (PM2.5) filter samples, size-resolved micro-orifice
uniform deposit impactor (MOUDI impactor) samples, and near-real-time analysis
by a newly acquired Particle into Liquid System (PILS). High-volume
samples were collected throughout the study for identification of organic
species using gas chromatography/mass spectrometry (GC/MS). Weekly study
composites have been analyzed to identify smoke markers, including levoglucosan,
that can apportion a fraction of the organic carbon (OC) mass to smoke-derived
aerosols. In addition we have identified significant concentrations
of several organic compounds that indicate an important contribution to secondary
organic aerosols from biogenic sources. We are also testing measurement
of levoglucosan, a wood smoke marker, in some of these samples by a newly
developed biosensor technique. New instruments run in the summer 2002
smoke study included a continuous carbon analyzer and a dual wavelength aethalometer.
Upcoming efforts will focus on relating these data to other Yosemite study
data sets and evaluating the ability of the instruments to detect the presence
of wood smoke on a near real-time basis. Collaboration is also ongoing
with Dr. Graham Bench of Lawrence Livermore National Laboratory. Dr.
Bench has analyzed the carbon isotope composition of several Yosemite samples
in order to evaluate relative contributions from “modern” vs. “fossil” carbon.
This approach, which suggests dominant contributions from biogenic carbon
sources, complements the organic speciation work.
IMPROVE Nitrate Study
Sponsor: National Park Service, Land and Water Fund of the Rockies
Project Period: September 2002 - August 2003
A series of field and laboratory studies was planned for 2003 and 2004 to
investigate characteristics of nitrate and other ions in aerosol particles
at selected, characteristic IMPROVE sites. These measurements are designed
to address the following issues:
- Does extraction of IMPROVE nylon filters with deionized water provide
efficient recovery of collected nitrate particles?
- Does collection of fine particles on nylon filters produce a negative
bias in ammonium concentrations, due to loss of volatilized ammonia, at IMPROVE
sites?
- What are the size distributions of nitrate, and other species, in aerosol
particles present at characteristic IMPROVE sites?
- What are the gas-particle distributions of nitric acid/nitrate and
ammonia/ammonium at selected IMPROVE sites?
In order to address these questions a series of six one month studies was
planned. The first four studies are being completed as part of our
2002-03 work. These include studies in Bondville, Illinois (Feb. 2003),
San Gorgonio Wilderness Area, California (April and July 2003) and Grand
Canyon National Park (May 2003). Additional studies are planned for
November 2003 in Brigantine, New Jersey and February 2004 in Sequoia National
Park. Measurements conducted for these studies include:
- Daily paired 24 hr denuder/filter/denuder setups to examine nylon filter
extraction via water vs. basic (IC extract) solution, ammonium loss from
nylon filters, and gas/particle partitioning of ammonia/ammonium and nitric
acid/nitrate. Major anions (NO3-, Cl-, SO42-) and cations (Na+, K+,
NH4+, Ca2+, Mg2+) are being examined as are gaseous ammonia and nitric acid.
- 12 hr denuder/filter/denuder setups to examine day/night differences
in gas-particle partitioning and ammonium loss.
- 48 hr MOUDI samples for anions and cations
- Semi-continuous measurements of PM2.5 aerosol anion and cation concentrations
using the PILS system. (PILS measurements were not originally planned
for these campaigns but were added due to their utility as demonstrated in
the Yosemite work).
In addition to these field studies, a series of lab experiments is being
conducted at CSU to investigate methods used by IMPROVE for nitrate measurement,
including issues related to denuder efficiency and filter extraction.
Specific investigations include:
- Local aerosol collection on denuded nylon filters and testing of nylon
filter extraction efficiency (by deionized water and by a sodium carbonate/sodium
bicarbonate solution).
- Tests of IMPROVE nitrate denuder efficiency for new and (field) exposed
denuders. Study of how denuder efficiency varies with relative humidity.
Chemical Heterogeneity Among Fog
Drop Populations and its Influence on Aerosol Processing by Fogs
Sponsor: National Science Foundation
Project Period: January 2000 - December 2003
Recent NSF sponsorship supported work leading to an increased understanding
of chemical heterogeneity present among cloud and fog drop populations and
the effects this heterogeneity exerts on aerosol and trace gas processing
by clouds and fogs. Significant effects on both formation of new aerosol
mass (via aqueous sulfur oxidation) and aerosol removal (via direct fog drop
deposition and by incorporation of cloud drops into precipitation) have been
noted. This grant also supported the design, construction, calibration and
field testing of two new cloud/fog samplers designed to provide better resolution
of drop composition as a function of drop size. A 3-stage collector
was developed for use in supercooled clouds while a 5-stage collector was
developed for use in warm clouds and fogs. These instruments represent
a significant advance over previous collector technology which permitted
the simultaneous collection of two drop size fractions. The performance
of the two new collectors was evaluated through a combination of numerical
modeling and laboratory calibration. Both collectors have also been
thoroughly tested in the field.
This project will apply the newly developed multi-stage collectors to better
characterize (in five drop size fractions rather than just two) chemical
heterogeneity present among fog drop populations and its influence on aerosol
formation and removal in fogs forming in polluted environments. Studies
of polluted fogs are planned because non-uniform drop chemistry appears to
exert the greatest effect on aerosol processing in this environment and because
an excellent opportunity exists to interface measurements with the upcoming
California Regional PM10/PM2.5 Air Quality Study (CRPAQS). The new
multi-stage collectors will be deployed to measure drop size-resolved fog
composition in two major field campaigns: in winter 2000/01 during the CRPAQS
winter intensive in California’s San Joaquin Valley and in winter 2001/02
in a study of aerosol processing by fogs in Denver’s Brown Cloud. Results
from both studies will represent a considerable advance in understanding of
how fog drop composition varies across the drop size spectrum and the influence
of this variation on aerosol formation (via gas uptake and aqueous sulfur
oxidation) and removal (via drop deposition). The CRPAQS study will
also provide the first good opportunity to test the ability of size-resolved
fog chemistry models to accurately predict the size-dependent chemical composition
of fogs. A new 2-stage stainless steel fog sampler will also be developed
and deployed in both field campaigns. This instrument will provide
the first reliable information about the distribution of organic carbon across
the drop size spectrum and its influence on the ability of urban fogs to
cleanse the atmosphere of organic aerosol particles by scavenging and deposition.
Measurement of Fog/Cloud Chemistry
and Gaeous Peroxides at the Pittsburgh PM2.5 Supersite
Sponsor: U.S. Environmental Protection Agency via sucontract
from Carnegie Mellon University
Project Period: July 2000 - June 2003
Colorado State University (CSU) will make two types of measurements at the
Pittsburgh Supersite. CSU, in conjunction with Carnegie Mellon researchers,
will make gas phase measurements of hydrogen peroxide and soluble organic
peroxides using a continuous monitor based on the method of Lazrus et al.
(1986). Expertise and instrumentation for the peroxide measurements will
be provided by CSU with day-to-day operation handled by CMU personnel.
Samples of fogs and low clouds will also be collected by CSU during a winter
intensive study. Operation of the cloud sampler will be automated for
this study. Fog/cloud presence will be detected using a Gerber Scientific
Particulate Volume Monitor. Collected fog/cloud samples will be analyzed
on-site for pH and sample aliquots will be prepared for later analysis of
major ion concentrations at CSU. A subset of samples will also be aliquotted
and stabilized for later analysis at CSU of total organic carbon (TOC), formaldehyde,
and trace metal catalysts (Fe and Mn).
Peroxide data will be used by other researchers to examine links between
peroxide concentrations and health effects. Peroxide and cloud/fog
data will be examined to elucidate the role of regional fogs and clouds on
aerosol production and removal. Rates and dominant pathways of aqueous
phase sulfate production will be determined as will efficiencies of aerosol
particle scavenging by clouds and fogs.
On-line determination of organic
compounds in atmospheric aerosols by direct impaction capillary electrophoresis
Sponsor: U.S. Department of Energy via subcontract from Aerosol
Dynamics, Inc.
Project Period: August 2002 - April 2003
Capillary electrophoresis (CE) is a recently developed technique that has
proven quite useful for analysis of various chemical species, including ions,
especially in small sample volumes. CE has the ability to readily separate
the mono- and dicarboxylic acids found in the particle phase. Elution
times for dicarboxcylic acids are a few minutes. Sample preparation
is simple by comparison to gas chromatographic methods that require derivatization
to enable the elution of these polar compounds. One disadvantage is that
CE is not quite as sensitive as ion chromatography. On the other hand, the
necessary injection volume is much smaller, approximately 10 nanoliters.
Thus, if one is able to handle the small injection volumes, very small samples
can be analyzed and the absolute amount of material required for analysis
is much smaller than with ion chromatography. Further, analysis by
CE can identify many more carboxylic and dicarboxylic acid compounds than
can ion chromatography.
In this proposal, we outline an approach for concentrating aerosol samples
in a small aqueous volume for the in-situ analysis of particle-bound carboxylic
acids. We propose a method based on humidification of the samples with collection
by impaction, and on-line analysis by capillary electrophoresis. This
proposal addresses the important need to know the origins, formation processes
and atmospheric life cycles of the oxygenated acids found in atmospheric
aerosols. Because these compounds tend to be hygroscopic, they may play an
important role in visibility and cloud formation. At present there is no
automated way to quantitatively measure these compounds in situ, with
high time resolution. The proposed instrument will provide a robust, economical
means to measure the concentrations of individual carboxylic acids on a routine
basis.
Development of an Airborne Cloud
Water Sampler
Sponsor: National Science Foundation
Project Period: March 2001 - February 2003
The objective of the proposed research is to develop, test and deploy an
aircraft based cloudwater collection system. The design will improve
upon previous aircraft-based collectors by offering an automated collection
system that is capable of obtaining multiple, well-characterized cloudwater
samples for chemical analysis. The system will feature a versatile design
that will be applicable to multiple research aircraft.
The initial design of the improved aircraft-based cloudwater collector is
currently underway. After an initial review process, an axial flow
cyclone design was chosen to provide efficient separation of cloud drops
from the ambient airstream. This design was selected for its ability to process
relatively large quantities of air in a compact space. The design consists
of a duct with a 6 cm diameter inlet that is exposed to the ambient airstream.
As incoming air encounters eight stationary, curved vanes within the duct,
the flow is redirected to produce a rotational flow field about the duct
centerline. Centrifugal force resulting from the rotational flow acts
to remove cloud drops to the duct wall, where they accumulate and are removed
through an extraction slot located downstream of the vanes.
The work to be completed under this proposal will be to continue the development
of the cloudwater collection system. The system will be taken from
the initial design and testing phases to the production of a final optimized
design suitable for deployment during future field campaigns. As the design
of the cloudwater collector progresses, numerical modeling will be used as
an ongoing design and analysis tool. Characterization of the flow in and
around the cloudwater collector and cloud drop trajectory simulations will
be performed with the Computational Fluid Dynamics (CFD) software package,
FLUENT v5.0. A finalized version of the cloudwater collector that incorporates
design modifications resulting from the initial testing phase, including
wind tunnel tests, and ongoing numerical fluid flow analysis will be assembled.
An automated sample storage system will also be developed as part of the
finalized design.
The collection system will then be deployed in an upcoming field study as
a final design test. Two field programs are being considered for possible
participation: the Asian Pacific Regional Aerosol Characterization Experiment
(ACE-Asia) study and the Megacity Impact on Regional and Global Environment
– Mexico City (MIRAGE – Mexico) study both have substantial cloud/aerosol
interaction components that would benefit from the ability to collect well-characterized
cloudwater samples. Chemical analysis of collected cloudwater samples
will be used to investigate the effects of cloud processing on aerosol particles
and the influence of aerosol physical and chemical properties on cloud formation.
This effort will help satisfy the cloud/aerosol objectives of the ACE – Asia
and MIRAGE – Mexico programs and provide data for cloud processing, chemical
transport, and radiative transfer models. MORE INFORMATION
Collett Research
Group Recent Projects
Application of a Tracer Technique
to Study Sulfur Dioxide Oxidation in Cloud Drops as a Function of Drop Size
Sponsor: National Science Foundation
Project Period: 12/1997 - 11/2000
Recent cloud chemistry models predict cloud drop composition varies with
drop size, a prediction confirmed by experimental measurements. Chemical heterogeneity
among cloud drop populations has the potential to significantly influence
aqueous phase sulfur oxidation. Drop acidity exerts a strong influence on
SO2 oxidation by O3. Both drop acidity and concentrations
of Fe(III) and Mn(II) affect the rate of trace metal catalyzed S(IV) autooxidation.
Observations of size-dependent cloud drop composition suggest that sulfur
oxidation by O3 and oxygen should vary with drop size in many
environments, typically favoring faster sulfate production in large drops.
Due to the non-linear nature of the oxidation rate laws for these pathways,
the average oxidation rate in a chemically heterogeneous cloud drop population
can also significantly exceed the rate expected from the average drop composition.
In environments where clouds are at least mildly acidic and H2O2
is present at concentrations comparable to or in excess of SO2,
H2O2 tends to be the dominant S(IV) oxidant. Observations
indicate that H2O2 concentrations do not vary with drop
size. Since the oxidation rate for this pathway does not depend on drop acidity
over an atmospherically relevant pH range, sulfate production rates are not
expected to vary with drop size when H2O2 is the dominant
oxidant.
Quantifying sulfur oxidation rates in ambient clouds has always been an
extremely difficult task. Recently developed tracer techniques, which examine
changes in the ratio of sulfate to a conservative aerosol tracer (Se, As,
or Sb) between pre-cloud aerosol and cloud water, however, have been demonstrated
capable of accurately quantifying aqueous phase sulfate production.
This project, conducted jointly by the cloud chemistry teams at Colorado
State University and at the State University of New York at Albany/ New York
State Department of Health, will test the hypothesis that sulfate production
does not vary with drop size when H2O2 is the dominant
oxidant, but can vary significantly with drop size when oxidation by O3
or trace metal catalyzed autooxidation are dominant. To this end, the study
will apply tracer techniques to measure sulfate production in large and small
cloud drops collected using a size-fractionating cloud collector. Measurements
of droplet composition and gaseous concentrations of SO2, O3
and H2O2 will also be made to permit prediction of
sulfur oxidation rates as a function of drop size for comparison with rates
determined by the tracer technique. Two environments (Whiteface Mountain,
New York, and Davis, California) have been selected for study to ensure that
conditions will be encountered where H2O2 is and is
not the dominant oxidant.
The study will confirm whether or not predicted variations in sulfate production
rates across the cloud drop size spectrum are borne out in real clouds. This
information is critical to assessing the need to track variations in drop
composition as a function of drop size in cloud chemistry models in order
to accurately represent rates of aqueous phase sulfate production and the
addition of sulfate mass to aerosol particles released by evaporating clouds.
MORE INFORMATION
Big Bend Regional Aerosol and
Visibility Observational (BRAVO) Study
Sponsor: National Park Service
Conducted jointly with S.M. Kredenweis
This project involves participation in the 1999 Big Bend Regional Aerosol
and Visibility Observational (BRAVO) Study. The overall project goal is to
examine the chemical composition, degree of internal mixing, and scattering
and absorption properties of aerosols at Big Bend National Park during July
– October, 1999. Air quality at the Park is believed to respond to transport
of aerosols and gases across the U.S.-Mexico border, thus our studies seek
to not only characterize the haze present at the site under different meteorological
conditions but to also apply methods that can help elucidate the sources
of particulate matter. Our measurements include organic and inorganic composition
of the fine aerosol, aerosol physical size distributions, and trace species
identification that will be used to generate a source apportionment of carbonaceous
aerosol at the study site. MORE INFORMATION
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