4.6 Article

Secondary Organic Aerosol Composition from C12 Alkanes

Journal

JOURNAL OF PHYSICAL CHEMISTRY A
Volume 119, Issue 19, Pages 4281-4297

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/jp501779w

Keywords

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Funding

  1. U.S. Department of Energy [DE-SC 0006626]
  2. National Science Foundation [AGS-1057183]
  3. Department of Defense Science, Mathematics, and Research for Transformation Fellowship
  4. Directorate For Geosciences
  5. Div Atmospheric & Geospace Sciences [1057183] Funding Source: National Science Foundation

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The effects of structure, NOx conditions, relative humidity, and aerosol acidity on the chemical composition of secondary organic aerosol (SOA) are reported for the photooxidation of three C-12 alkanes: n-dodecane, cyclododecane, and hexylcyclohexane. Acidity was modified through seed particle composition: NaCl, (NH4)(2)SO4, and (NH4)(2)SO4 + H2SO4. Off-line analysis of SOA was carried out by solvent extraction and gas chromatography-mass spectrometry (GC/MS) and direct analysis in real-time mass spectrometry. We report here 750 individual masses of SOA products identified from these three alkane systems and 324 isomers resolved by GC/MS analysis. The chemical compositions for each alkane system provide compelling evidence of particle-phase chemistry, including reactions leading to oligomer formation. Major oligomeric species for alkane SOA are peroxyhemiacetals, hemiacetals, esters, and aldol condensation products. Furans, dihydrofurans, hydroxycarbonyls, and their corresponding imine analogues are important participants in these oligomer-producing reactions. Imines are formed in the particle phase from the reaction of the ammonium sulfate seed aerosol with carbonyl-bearing compounds present in all the SOA systems. Under high-NO conditions, organonitrate products can lead to an increase of aerosol volume concentration by up to a factor of 5 over that in low-NO conditions. Structure was found to play a key role in determining the degree of functionalization and fragmentation of the parent alkane, influencing the mean molecular weight of the SOA produced and the mean atomic O:C ratio.

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