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The formation of secondary organic aerosol from the isoprene + OH reaction in the absence of NO

Atmospheric Chemistry and Physics, ISSN: 1680-7324, Vol: 9, Issue: 17, Page: 6541-6558
2009
  • 102
    Citations
  • 0
    Usage
  • 88
    Captures
  • 0
    Mentions
  • 0
    Social Media
Metric Options:   Counts1 Year3 Year

Metrics Details

  • Citations
    102
    • Citation Indexes
      102
  • Captures
    88

Article Description

The reaction of isoprene (CH) with hydroxyl radicals has been studied in the absence of nitrogen oxides (NO) to determine physical and chemical characteristics of the secondary organic aerosol formed. Experiments were conducted using a smog chamber operated in a steady-state mode permitting measurements of moderately low aerosol levels. GC-MS analysis was conducted to measure methyl butenediols in the gas phase and polyols in the aerosol phase. Analyses were made to obtain several bulk aerosol parameters from the reaction including values for the organic mass to organic carbon ratio, the effective enthalpy of vaporization ( ΔH ), organic peroxide fraction, and the aerosol yield.The gas phase analysis showed the presence of methacrolein, methyl vinyl ketone, and four isomers of the methyl butenediols. These gas-phase compounds may serve as precursors for one or more of several compounds detected in the aerosol phase including 2-methylglyceric acid, three 2methyl alkenetriols, and two 2-methyl tetrols. In contrast to most previous studies, the 2-methyl tetrols (and the 2-methyl alkenetriols) were found to form in the absence of acidic sulfate aerosol. However, reaction conditions did not favor the production of HO radicals, thus allowing RO+RO reactions to proceed more readily than if higher HO levels had been generated.SOA/SOC (i.e. OM/OC) was found to average 1.9 in the absence of NO. The effective enthalpy of vaporization was measured as 38.6 kJ mol, consistent with values used previously in modeling studies. The yields in this work (us- ing an independent technique than used previously) are lower than those of Kroll et al. (2006) for similar aerosol masses. SOC yields reported in this work range from 0.5-1.4% for carbon masses between 17 and 49μgC m.

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