Details

Autor(en) / Beteiligte

• Lee, Ben H.
• Mohr, Claudia
• Lopez-Hilfiker, Felipe D.
• Lutz, Anna
• Hallquist, Mattias
• Lee, Lance
• Romer, Paul
• Cohen, Ronald C.
• Iyer, Siddharth
• Kurtén, Theo
• Hu, Weiwei
• Day, Douglas A.
• Campuzano-Jost, Pedro
• Jimenez, Jose L.
• Xu, Lu
• Ng, Nga Lee
• Guo, Hongyu
• Weber, Rodney J.
• Wild, Robert J.
• Brown, Steven S.
• Koss, Abigail
• de Gouw, Joost
• Olson, Kevin
• Goldstein, Allen H.
• Seco, Roger
• Kim, Saewung
• McAvey, Kevin
• Shepson, Paul B.
• Starn, Tim
• Baumann, Karsten
• Edgerton, Eric S.
• Liu, Jiumeng
• Shilling, John E.
• Miller, David O.
• Brune, William
• Schobesberger, Siegfried
• D’Ambro, Emma L.
• Thornton, Joel A.

Titel

Highly functionalized organic nitrates in the southeast United States: Contribution to secondary organic aerosol and reactive nitrogen budgets

Ist Teil von

• Proceedings of the National Academy of Sciences - PNAS, 2016-02, Vol.113 (6), p.1516-1521

Ort / Verlag

United States: National Academy of Sciences

Erscheinungsjahr

2016

Link zum Volltext

Quelle

EZB Free E-Journals

Beschreibungen/Notizen

• Speciated particle-phase organic nitrates (pONs) were quantified using online chemical ionization MS during June and July of 2013 in rural Alabama as part of the Southern Oxidant and Aerosol Study. A large fraction of pONs is highly functionalized, possessing between six and eight oxygen atoms within each carbon number group, and is not the common first generation alkyl nitrates previously reported. Using calibrations for isoprene hydroxynitrates and the measured molecular compositions, we estimate that pONs account for 3% and 8% of total submicrometer organic aerosol mass, on average, during the day and night, respectively. Each of the isoprene- and monoterpenes-derived groups exhibited a strong diel trend consistent with the emission patterns of likely biogenic hydrocarbon precursors. An observationally constrained diel box model can replicate the observed pON assuming that pONs (i) are produced in the gas phase and rapidly establish gas–particle equilibrium and (ii) have a short particle-phase lifetime (∼2–4 h). Such dynamic behavior has significant implications for the production and phase partitioning of pONs, organic aerosol mass, and reactive nitrogen speciation in a forested environment.