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Detailed Reference Information |
Broekhuizen, K.E., Thornberry, T., Kumar, P.P. and Abbatt, J.P.D. (2004). Formation of cloud condensation nuclei by oxidative processing: Unsaturated fatty acids. Journal of Geophysical Research 109: doi: 10.1029/2004JD005298. issn: 0148-0227. |
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The ability of submicron oleic acid and linoleic acid particles, or condensation nuclei (CN), to act as cloud condensation nuclei (CCN) has been investigated using a tandem differential mobility analyzer (TDMA) coupled to a flow tube reactor and a thermal gradient diffusion chamber (TGDC). The size change and CCN properties of pure oleic acid, mixed oleic acid/methanol, and pure linoleic acid particles have been investigated as a function of exposure to ozone. Pure oleic and linoleic acid particles were CCN inactive for all particle diameters (≤300 nm) and supersaturations (≤1%) studied. The mixed oleic acid/methanol particles, however, had a critical activation diameter of 188 nm for an experimental water supersaturation of 0.6%. Under low ozone exposures (<1 ¿ 10-4 atm s), both the oleic acid and linoleic acid particles decreased in size. In particular, oleic acid particles lost 25% of their initial volume, consistent with the loss of nonanal, a volatile reaction product. However, no increase in CCN activity was observed at these exposures. Under conditions of much higher ozone exposure, e.g., 0.42 atm s, the pure oleic acid particles became CCN active, with a critical activation diameter of 161 nm at 0.6% supersaturation. CCN activity for the linoleic acid particles was never observed, even under these high ozone exposures not typically observed in the atmosphere. By contrast, the mixed oleic acid/methanol particles showed enhanced activation under atmospherically relevant ozone exposures (<1 ¿ 10-4 atm s). These results suggest that the products of the ozone plus unsaturated fatty acid reaction do promote the CCN activity of the particles; however, the degree of activity is dependent on both the level of ozone exposure and the chemical nature of the particle. These results are the first to demonstrate that the CCN properties of pure organic aerosols can be modified through oxidative processing. |
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Abstract |
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Keywords
Atmospheric Composition and Structure, Aerosols and particles (0345, 4801), Atmospheric Composition and Structure, Cloud physics and chemistry, Atmospheric Composition and Structure, Pollution—urban and regional, CCN, organic aerosols, ozone, oleic acid, oxidative processing |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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