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Atmos. Meas. Tech., 10, 2283-2298, 2017
https://doi.org/10.5194/amt-10-2283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
22 Jun 2017
Controlled nitric oxide production via O(1D)  + N2O reactions for use in oxidation flow reactor studies
Andrew Lambe1,2, Paola Massoli1, Xuan Zhang1,a, Manjula Canagaratna1, John Nowak1,b, Conner Daube1, Chao Yan3, Wei Nie4,3, Timothy Onasch1,2, John Jayne1, Charles Kolb1, Paul Davidovits2, Douglas Worsnop1,3, and William Brune5 1Aerodyne Research, Inc., Billerica, Massachusetts, USA
2Chemistry Department, Boston College, Chestnut Hill, Massachusetts, USA
3Physics Department, University of Helsinki, Helsinki, Finland
4Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University, Nanjing, China
5Department of Meteorology and Atmospheric Sciences, The Pennsylvania State University, University Park, Pennsylvania, USA
aCurrent address: Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, Colorado, USA
bCurrent address: Chemistry and Dynamics Branch, NASA Langley Research Center, Hampton, Virginia, USA
Abstract. Oxidation flow reactors that use low-pressure mercury lamps to produce hydroxyl (OH) radicals are an emerging technique for studying the oxidative aging of organic aerosols. Here, ozone (O3) is photolyzed at 254 nm to produce O(1D) radicals, which react with water vapor to produce OH. However, the need to use parts-per-million levels of O3 hinders the ability of oxidation flow reactors to simulate NOx-dependent secondary organic aerosol (SOA) formation pathways. Simple addition of nitric oxide (NO) results in fast conversion of NOx (NO + NO2) to nitric acid (HNO3), making it impossible to sustain NOx at levels that are sufficient to compete with hydroperoxy (HO2) radicals as a sink for organic peroxy (RO2) radicals. We developed a new method that is well suited to the characterization of NOx-dependent SOA formation pathways in oxidation flow reactors. NO and NO2 are produced via the reaction O(1D) + N2O  →  2NO, followed by the reaction NO + O3  →  NO2 + O2. Laboratory measurements coupled with photochemical model simulations suggest that O(1D) + N2O reactions can be used to systematically vary the relative branching ratio of RO2 + NO reactions relative to RO2 + HO2 and/or RO2 + RO2 reactions over a range of conditions relevant to atmospheric SOA formation. We demonstrate proof of concept using high-resolution time-of-flight chemical ionization mass spectrometer (HR-ToF-CIMS) measurements with nitrate (NO3) reagent ion to detect gas-phase oxidation products of isoprene and α-pinene previously observed in NOx-influenced environments and in laboratory chamber experiments.

Citation: Lambe, A., Massoli, P., Zhang, X., Canagaratna, M., Nowak, J., Daube, C., Yan, C., Nie, W., Onasch, T., Jayne, J., Kolb, C., Davidovits, P., Worsnop, D., and Brune, W.: Controlled nitric oxide production via O(1D)  + N2O reactions for use in oxidation flow reactor studies, Atmos. Meas. Tech., 10, 2283-2298, https://doi.org/10.5194/amt-10-2283-2017, 2017.
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Short summary
This work enables the study of NOx-influenced secondary organic aerosol formation chemistry in oxidation flow reactors to an extent that was not previously possible. The method uses reactions of exited oxygen O(1D) radicals (formed from ozone photolysis at 254 nm or nitrous oxide photolysis at 185 nm) with nitrous oxide (N2O) to produce NO. We demonstrate proof of concept using chemical ionization mass spectrometer measurements to detect gas-phase oxidation products of isoprene and α-pinene.
This work enables the study of NOx-influenced secondary organic aerosol formation chemistry in...
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