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Secondary organic aerosol formation from cyclohexene ozonolysis in the presence of water vapor and dissolved salts
AbstractA series of 90 experiments were conducted in the UC Riverside/CE-CERT environmental chamber to evaluate the impact of water vapor and dissolved salts on secondary organic aerosol formation for cyclohexene ozonolysis. Water vapor (low – 30±2% RH, medium – 46±2% RH, high – 63±2% RH) was found to directly participate in the atmospheric chemistry altering the composition of the condensing species, thus increasing total organic aerosol formation by ∼22% as compared to the system under dry (<0.1% RH) conditions. Hygroscopicity measurements also indicate that the organic aerosol composition is altered in the presence of gaseous water. These results are consistent with water vapor reacting with the crigee intermediate in the gas phase resulting in increased aldehyde formation. The addition of dissolved salts ((NH4)2SO4, NH4HSO4, CaCl2, NaCl) had minimal effect; only the (NH4)2SO4 and NaCl were found to significantly impact the system with ∼10% increase in total organic aerosol formation. These results indicate that the organics may be partitioning to an outer organic shell as opposed to into the aqueous salt. Hygroscopicity measurements indicate that the addition of salts does not alter the aerosol composition for the dry or water vapor system.
Secondary organic aerosol formation from cyclohexene ozonolysis in the presence of water vapor and dissolved salts
AbstractA series of 90 experiments were conducted in the UC Riverside/CE-CERT environmental chamber to evaluate the impact of water vapor and dissolved salts on secondary organic aerosol formation for cyclohexene ozonolysis. Water vapor (low – 30±2% RH, medium – 46±2% RH, high – 63±2% RH) was found to directly participate in the atmospheric chemistry altering the composition of the condensing species, thus increasing total organic aerosol formation by ∼22% as compared to the system under dry (<0.1% RH) conditions. Hygroscopicity measurements also indicate that the organic aerosol composition is altered in the presence of gaseous water. These results are consistent with water vapor reacting with the crigee intermediate in the gas phase resulting in increased aldehyde formation. The addition of dissolved salts ((NH4)2SO4, NH4HSO4, CaCl2, NaCl) had minimal effect; only the (NH4)2SO4 and NaCl were found to significantly impact the system with ∼10% increase in total organic aerosol formation. These results indicate that the organics may be partitioning to an outer organic shell as opposed to into the aqueous salt. Hygroscopicity measurements indicate that the addition of salts does not alter the aerosol composition for the dry or water vapor system.
Secondary organic aerosol formation from cyclohexene ozonolysis in the presence of water vapor and dissolved salts
Warren, Bethany (author) / Malloy, Quentin G.J. (author) / Yee, Lindsay D. (author) / Cocker, David R. III (author)
Atmospheric Environment ; 43 ; 1789-1795
2008-12-16
7 pages
Article (Journal)
Electronic Resource
English
A chamber study of secondary organic aerosol formation by limonene ozonolysis
| Wiley | 2010