Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011

At the Rocky Mountain Biogenic Aerosol Study (BEACHON-RoMBAS) field campaign in the Colorado front range, July–August 2011, measurements of gas- and aerosol-phase organic nitrates enabled a study of the role of NO<sub>x</sub> (NO<sub>x</sub> = NO + NO<sub>2</sub>)...

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Main Authors: J. L. Fry, D. C. Draper, K. J. Zarzana, P. Campuzano-Jost, D. A. Day, J. L. Jimenez, S. S. Brown, R. C. Cohen, L. Kaser, A. Hansel, L. Cappellin, T. Karl, A. Hodzic Roux, A. Turnipseed, C. Cantrell, B. L. Lefer, N. Grossberg
Format: Article
Language:English
Published: Copernicus Publications 2013-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/8585/2013/acp-13-8585-2013.pdf
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author J. L. Fry
D. C. Draper
K. J. Zarzana
P. Campuzano-Jost
D. A. Day
J. L. Jimenez
S. S. Brown
R. C. Cohen
L. Kaser
A. Hansel
L. Cappellin
T. Karl
A. Hodzic Roux
A. Turnipseed
C. Cantrell
B. L. Lefer
N. Grossberg
author_facet J. L. Fry
D. C. Draper
K. J. Zarzana
P. Campuzano-Jost
D. A. Day
J. L. Jimenez
S. S. Brown
R. C. Cohen
L. Kaser
A. Hansel
L. Cappellin
T. Karl
A. Hodzic Roux
A. Turnipseed
C. Cantrell
B. L. Lefer
N. Grossberg
author_sort J. L. Fry
collection DOAJ
description At the Rocky Mountain Biogenic Aerosol Study (BEACHON-RoMBAS) field campaign in the Colorado front range, July–August 2011, measurements of gas- and aerosol-phase organic nitrates enabled a study of the role of NO<sub>x</sub> (NO<sub>x</sub> = NO + NO<sub>2</sub>) in oxidation of forest-emitted volatile organic compounds (VOCs) and subsequent aerosol formation. Substantial formation of peroxy- and alkyl-nitrates is observed every morning, with an apparent 2.9% yield of alkyl nitrates from daytime RO<sub>2</sub> + NO reactions. <i>Aerosol-phase</i> organic nitrates, however, peak in concentration during the night, with concentrations up to 140 ppt as measured by both optical spectroscopic and mass spectrometric instruments. The diurnal cycle in aerosol fraction of organic nitrates shows an equilibrium-like response to the diurnal temperature cycle, suggesting some reversible absorptive partitioning, but the full dynamic range cannot be reproduced by thermodynamic repartitioning alone. Nighttime aerosol organic nitrate is observed to be positively correlated with [NO<sub>2</sub>] × [O<sub>3</sub>] but not with [O<sub>3</sub>]. These observations support the role of nighttime NO<sub>3</sub>-initiated oxidation of monoterpenes as a significant source of nighttime aerosol. Nighttime production of organic nitrates is comparable in magnitude to daytime photochemical production at this site, which we postulate to be representative of the Colorado front range forests.
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spelling doaj.art-13aa829563da4b28ac9fc29f99403b142022-12-22T01:27:08ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-09-0113178585860510.5194/acp-13-8585-2013Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011J. L. FryD. C. DraperK. J. ZarzanaP. Campuzano-JostD. A. DayJ. L. JimenezS. S. BrownR. C. CohenL. KaserA. HanselL. CappellinT. KarlA. Hodzic RouxA. TurnipseedC. CantrellB. L. LeferN. GrossbergAt the Rocky Mountain Biogenic Aerosol Study (BEACHON-RoMBAS) field campaign in the Colorado front range, July–August 2011, measurements of gas- and aerosol-phase organic nitrates enabled a study of the role of NO<sub>x</sub> (NO<sub>x</sub> = NO + NO<sub>2</sub>) in oxidation of forest-emitted volatile organic compounds (VOCs) and subsequent aerosol formation. Substantial formation of peroxy- and alkyl-nitrates is observed every morning, with an apparent 2.9% yield of alkyl nitrates from daytime RO<sub>2</sub> + NO reactions. <i>Aerosol-phase</i> organic nitrates, however, peak in concentration during the night, with concentrations up to 140 ppt as measured by both optical spectroscopic and mass spectrometric instruments. The diurnal cycle in aerosol fraction of organic nitrates shows an equilibrium-like response to the diurnal temperature cycle, suggesting some reversible absorptive partitioning, but the full dynamic range cannot be reproduced by thermodynamic repartitioning alone. Nighttime aerosol organic nitrate is observed to be positively correlated with [NO<sub>2</sub>] × [O<sub>3</sub>] but not with [O<sub>3</sub>]. These observations support the role of nighttime NO<sub>3</sub>-initiated oxidation of monoterpenes as a significant source of nighttime aerosol. Nighttime production of organic nitrates is comparable in magnitude to daytime photochemical production at this site, which we postulate to be representative of the Colorado front range forests.http://www.atmos-chem-phys.net/13/8585/2013/acp-13-8585-2013.pdf
spellingShingle J. L. Fry
D. C. Draper
K. J. Zarzana
P. Campuzano-Jost
D. A. Day
J. L. Jimenez
S. S. Brown
R. C. Cohen
L. Kaser
A. Hansel
L. Cappellin
T. Karl
A. Hodzic Roux
A. Turnipseed
C. Cantrell
B. L. Lefer
N. Grossberg
Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011
Atmospheric Chemistry and Physics
title Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011
title_full Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011
title_fullStr Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011
title_full_unstemmed Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011
title_short Observations of gas- and aerosol-phase organic nitrates at BEACHON-RoMBAS 2011
title_sort observations of gas and aerosol phase organic nitrates at beachon rombas 2011
url http://www.atmos-chem-phys.net/13/8585/2013/acp-13-8585-2013.pdf
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