HR: 1330h
AN: A32A-0113 [PDF]
TI: A Measurement of Gaseous and Particulate Biogenic Semi-Volatile Organic Compounds in the Forest
Atmosphere with an Annular Denuder Sampling System
AU: * Matsunaga, S
EM: smatsu@ucar.edu
AF: Atmospheric Chemistry Division,
National Center for Atmospheric Research, 1850 Table Mesa Drive, Boulder, CO 80303 United States
AU: * Matsunaga, S
EM: smatsu@ucar.edu
AF: Faculty of Engineering,
Tokyo Metropolitan University, 1-1 Minami-Osawa, Hachioji, 192-0364
Japan
AU: * Matsunaga, S
EM: smatsu@ucar.edu
AF: Institute of Low Temperature Science,
Hokkaido University, N19W8 Kita-Ku, Sapporo, 060-0819
Japan
AU: * Matsunaga, S
EM: smatsu@ucar.edu
AF: Graduate School of Environmental Earth Science,
Hokkaido University, N10W5 Kita-Ku, Sapporo, 060-0810
Japan
AU: Mochida, M
EM: mochida@pop.lowtem.hokudai.ac.jp
AF: Institute of Low Temperature Science,
Hokkaido University, N19W8 Kita-Ku, Sapporo, 060-0819
Japan
AU: Guenther, A B
EM: guenther@ucar.edu
AF: Atmospheric Chemistry Division,
National Center for Atmospheric Research, 1850 Table Mesa Drive, Boulder, CO 80303 United States
AU: Schnell, R
EM: ryan@ucar.edu
AF: Atmospheric Chemistry Division,
National Center for Atmospheric Research, 1850 Table Mesa Drive, Boulder, CO 80303 United States
AU: Greenberg, J
EM: greenber@ucar.edu
AF: Atmospheric Chemistry Division,
National Center for Atmospheric Research, 1850 Table Mesa Drive, Boulder, CO 80303 United States
AU: Kawamura, K
EM: kawamura@pop.lowtem.hokudai.ac.jp
AF: Institute of Low Temperature Science,
Hokkaido University, N19W8 Kita-Ku, Sapporo, 060-0819
Japan
AU: Kajii, Y
EM: kajii@atmchem.apchem.metro-u.ac.jp
AF: Faculty of Engineering,
Tokyo Metropolitan University, 1-1 Minami-Osawa, Hachioji, 192-0364
Japan
AB:
Atmospheric concentrations of biogenic semi-volatile organic compounds (SOCs) in both gas and particle phase have been
measured in two experimental forests with an annular denuder sampling system. The sampling sites were an experimental forest
of Hokkaido University at Moshiri in Hokkaido Island, northern Japan (from August 22 to 29, 2002) and an experimental forest
of Duke University at Chapel Hill in North Carolina, east coast of the United States (from July 9 to 12, 2003). The compounds
detected in the forest atmosphere are glycolaldehyde, hydroxyacetone, n-nonanal, n-decanal, glyoxal, methylglyoxal and
4-oxopental. Glycolaldehyde, hydroxyacetone and methylglyoxal are known as oxidation products of isoprene which has the
largest emission rate of any hydrocarbon species. Nonanal and decanal are probably directly emitted from vegetation.
4-oxopentanal is an oxidation product of 6-methyl-5-hepten-2-one. This is an oxidation product of organic compounds which are
abundant on plant surfaces. All of these compounds were detected in both gas and particle phases. Their concentrations
ranged from the detection limit (approximately 1 pptv) to 154 pptv (630 ng m-3, 4-oxopentanal), and the particulate
concentrations ranged from the detection limit (approximately 3 ng m-3) to 200 ng m-3 (4-oxopentanal) in Moshiri, 2002.
The gaseous concentrations of these compounds showed a clear diurnal variation on fine days. Although their production
processes are different each other, the variation showed the same pattern which was quite similar to the ambient temperature.
On the other hand, partition ratios (particle/(gas+particle)) of these compounds suggested that the process of
gas-to-particle conversion of these SOCs is different between water soluble compounds and insoluble compounds. The partition
ratios of water soluble compounds such as glycolaldehyde, hydroxyacetone and 4-oxopentanal (their Henry_fs constant exceed
10000 mol kg-1 atm-1) depends on relative humidity at the sampling site. This result suggested that water soluble SOCs can
convert into particles via dissolution into aerosols existing in the atmosphere, and this is a particular process for the
soluble SOCs.
In this presentation, we will compare the emission and removal processes of biogenic SOCs in the forest atmosphere of
Northern Japan with those in the East Coast of the United States. The observed SOCs behavior at the Duke Forest site is
compared with VOCs and aerosol chemical composition observed by other investigators during the CELTIC study.
DE: 0300 ATMOSPHERIC COMPOSITION AND STRUCTURE
DE: 0305 Aerosols and particles (0345, 4801)
DE: 0315 Biosphere/atmosphere interactions
DE: 0322 Constituent sources and sinks
DE: 1055 Organic geochemistry
SC: Atmospheric Sciences [A]
MN: 2003 Fall Meeting