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Detailed Reference Information |
Wyslouzil, B.E., Carleton, K.L., Sonnenfroh, D.M., Rawlins, W.T. and Arnold, S. (1994). Observation of hydration of single, modified carbon aerosols. Geophysical Research Letters 21: doi: 10.1029/94GL01588. issn: 0094-8276. |
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We have compared the hydration behavior of single carbon particles that have been treated by exposure to gaseous H2SO4 with that of untreated particles. Untreated carbon particles did not hydrate as the relative humidity varied from 0 to 80% at 23¿C. In contrast, treated particles hydrated under subsaturation conditions; mass increases of up to 30% were observed. The mass increase is consistent with sulfuric acid equilibration with the ambient relative humidity in the presence of inert carbon. For the samples studied, the average amount of adsorbed acid was 14%¿6% by weight, which corresponds to a surface coverage of ~0.1 monolayer. The mass fraction of surface-adsorbed acid is comparable to the soluble mass fraction observed by Whitefield et al. (1993) in jet aircraft engine aerosols. Estimates indicate this mass fraction corresponds to 0.1% of the available SO2 exiting an aircraft engine ending up as H2SO4 on the carbon aerosol. If this heterogeneous process occurs early enough in the exhaust plume, it may compete with homogeneous nucleation as a mechanism for producing sulfuric acid rich aerosols. ¿ American Geophysical Union 1994 |
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Abstract |
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Keywords
Atmospheric Composition and Structure, Aerosols and particles, Atmospheric Composition and Structure, Instruments and techniques, Atmospheric Composition and Structure, Troposphere—composition and chemistry, Atmospheric Composition and Structure, Cloud physics and chemistry |
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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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