Atmospheric Chemistry and Physics (Dec 2015)

Organic nitrate aerosol formation via NO<sub>3</sub> + biogenic volatile organic compounds in the southeastern United States

  • B. R. Ayres,
  • H. M. Allen,
  • D. C. Draper,
  • S. S. Brown,
  • R. J. Wild,
  • J. L. Jimenez,
  • D. A. Day,
  • P. Campuzano-Jost,
  • W. Hu,
  • J. de Gouw,
  • A. Koss,
  • R. C. Cohen,
  • K. C. Duffey,
  • P. Romer,
  • K. Baumann,
  • E. Edgerton,
  • S. Takahama,
  • J. A. Thornton,
  • B. H. Lee,
  • F. D. Lopez-Hilfiker,
  • C. Mohr,
  • P. O. Wennberg,
  • T. B. Nguyen,
  • A. Teng,
  • A. H. Goldstein,
  • K. Olson,
  • J. L. Fry

DOI
https://doi.org/10.5194/acp-15-13377-2015
Journal volume & issue
Vol. 15, no. 23
pp. 13377 – 13392

Abstract

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Gas- and aerosol-phase measurements of oxidants, biogenic volatile organic compounds (BVOCs) and organic nitrates made during the Southern Oxidant and Aerosol Study (SOAS campaign, Summer 2013) in central Alabama show that a nitrate radical (NO3) reaction with monoterpenes leads to significant secondary aerosol formation. Cumulative losses of NO3 to terpenes are correlated with increase in gas- and aerosol-organic nitrate concentrations made during the campaign. Correlation of NO3 radical consumption to organic nitrate aerosol formation as measured by aerosol mass spectrometry and thermal dissociation laser-induced fluorescence suggests a molar yield of aerosol-phase monoterpene nitrates of 23–44 %. Compounds observed via chemical ionization mass spectrometry (CIMS) are correlated to predicted nitrate loss to BVOCs and show C10H17NO5, likely a hydroperoxy nitrate, is a major nitrate-oxidized terpene product being incorporated into aerosols. The comparable isoprene product C5H9NO5 was observed to contribute less than 1 % of the total organic nitrate in the aerosol phase and correlations show that it is principally a gas-phase product from nitrate oxidation of isoprene. Organic nitrates comprise between 30 and 45 % of the NOy budget during SOAS. Inorganic nitrates were also monitored and showed that during incidents of increased coarse-mode mineral dust, HNO3 uptake produced nitrate aerosol mass loading at a rate comparable to that of organic nitrate produced via NO3 + BVOCs.