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1.
Size distributions and formation mechanisms of water-soluble organic
aerosols in a coastal environment
Jian
Zhen Yu
Department of Chemistry, Hong Kong University
of Science & Technology, Clear Water Bay, Kowloon, Hong
Kong
Phone: 852-2358-7389, fax: 852-2358-1594, email: chjianyu@ust.hk
Aerosol mass size distributions of water-soluble organic carbon
(WSOC) were studied at a coastal site in Hong Kong. Eleven sets
of 72-hr samples were collected using an 8-stage impactor sampler
over three seasons in 2000-2001. Regardless of air mass origins
being mainly marine or continental, WSOC exhibited bimodal size
distributions with a dominant fine mode and a minor coarse mode
in the size range of > 0.43 mm. The two modes had a mass mean
aerodynamic diameter (MMAD) of 0.7 ± 0.1 mm and 4.0 ±
0.3 mm, respectively. The fine WSOC accounted for the major proportion
of the total WSOC, ranging from two-thirds to four-fifths. The
WSOC mixtures were resolved into 3 to 5 peaks under controlled
progressive heating and combustion conditions. A positive matrix
factorization analysis deconvoluted the WSOC mixtures into three
component groups of different thermal behaviors. The three groups
of WSOC species were postulated to be low, medium, and high molecular
weight (MW) polar compounds on the basis of their thermal evolution
features. On average, they accounted for 21%, 39%, and 40% of
fine WSOC (<2.1 mm) mass, respectively. Coarse WSOC (>2.1
mm) was largely made of the low MW polar compound group. The low
MW group had a bimodal distribution with a dominant coarse mode,
likely associated with sea salt aerosols. The medium and the high
MW groups had a single mode distribution in the droplet mode,
both with an average MMAD of 0.7 ± 0.1 mm. Their droplet
mode presence indicated that they were associated with cloud-processed
particles. There is evidence to suggest that the high MW group
was likely secondary in origin, formed during cloud processing.
Key
Words: Water-soluble organic compounds,
Formation mechanisms, Cloud processing, Positive matrix factorization,
Secondary organic aerosols.
2.
Characterization of low molecular weight carboxylic acids in atmospheric
aerosols using capillary electrophoresis
Xiao-Ying
Yu*a, Susanne V. Hering c, Jeffrey L. Collett, Jr.a, and Charles
Henryb
a
Colorado State University, Department of Atmospheric Science,
Fort Collins, CO 80523-1371
b Colorado State University, Department of Chemistry, Fort Collins,
CO 80523-1872
c Aerosol Dynamics Inc., 2329 Fourth Street, Berkeley, CA 94710
Low
molecular weight carboxylic and dicarboxylic acids are important
airborne carbonaceous pollutants. They are found in a variety
of marine and continental environments. Some of these compounds
contribute to ambient and precipitation acidity and some are good
indicators of secondary organic aerosol production. Therefore,
the capability to measure atmospheric concentrations of these
species with high time resolution would greatly aid our understanding
of organic acid sources and effects.
By
applying high voltage across the length of an electrolyte-filled
capillary, different ions can be separated depending on their
size and charge. Capillary electrophoresis (CE) is considered
to be a powerful tool in environmental applications due to its
high efficiency, speed, small analyte mass requirements, and economy
of analysis. However, the use of CE so far in atmospheric chemistry
has been quite limited. In order to take advantage of the small
analyte mass requirement and efficient separation capabilities
of CE for semi-continuous characterization, collaboration between
Colorado State University (CSU) and Aerosol Dynamics Inc. (ADI)
was initiated.
Using
an analytical method based on indirect uv-vis detection [Dabek-Zlotorzynska
et al, 2001] more than a dozen low molecular weight carboxylic
acids can be separated in less than I 0 minutes with a detection
limit better than 1 µm. For aerosol measurement, this analytical
approach was used for samples collected by impaction, with direct
extraction from the collection surface. To attain high collection
rates with small particle cutoffs, particles are enlarged by water
condensation in a laminar, thermally diffusive flow (ADI, patent
pending). In work reported here, CE analysis of laboratory and
ambient aerosol samples was achieved with aqueous aerosol extracts
of I µm, or less, from aerosol particles deposited on different
substrate materials.
Preliminary
results of low molecular weight carboxylic and dicarboxylic acid
measurements from this prototype system are presented. The observed
ability to distinctly separate organic anions in ambient aerosol
samples utilizing I µL, injection indicate that the approach
is capable of monitoring atmospheric relevant carboxylic and dicarboxylic
acids. By changing separation and detection schemes, the system
can be readily adapted to measure other organic and inorganic
compounds as well. The combined system promises to provide a powerful
new technique for continuous aerosol composition measurement in
the future.
References
Dabek-Zlotorzynska, E., M. Piechowski, M. McGrath,
and E.P.C Lai, Determination of low-molecular-mass carboxylic
acids in atmospheric aerosol and vehicle emission samples by capillary
electrophoresis, J. Chromatogr. A, 910, 331-45, 2001.
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