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Organic nitrate chemistry and its implications for nitrogen budgets in an isoprene- and monoterpene-rich atmosphere: constraints from aircraft (SEAC4RS) and ground-based (SOAS) observations in the Southeast US.


ABSTRACT: Formation of organic nitrates (RONO2) during oxidation of biogenic volatile organic compounds (BVOCs: isoprene, monoterpenes) is a significant loss pathway for atmospheric nitrogen oxide radicals (NOx), but the chemistry of RONO2 formation and degradation remains uncertain. Here we implement a new BVOC oxidation mechanism (including updated isoprene chemistry, new monoterpene chemistry, and particle uptake of RONO2) in the GEOS-Chem global chemical transport model with ?25 × 25 km2 resolution over North America. We evaluate the model using aircraft (SEAC4RS) and ground-based (SOAS) observations of NOx, BVOCs, and RONO2 from the Southeast US in summer 2013. The updated simulation successfully reproduces the concentrations of individual gas- and particle-phase RONO2 species measured during the campaigns. Gas-phase isoprene nitrates account for 25-50% of observed RONO2 in surface air, and we find that another 10% is contributed by gas-phase monoterpene nitrates. Observations in the free troposphere show an important contribution from long-lived nitrates derived from anthropogenic VOCs. During both campaigns, at least 10% of observed boundary layer RONO2 were in the particle phase. We find that aerosol uptake followed by hydrolysis to HNO3 accounts for 60% of simulated gas-phase RONO2 loss in the boundary layer. Other losses are 20% by photolysis to recycle NOx and 15% by dry deposition. RONO2 production accounts for 20% of the net regional NOx sink in the Southeast US in summer, limited by the spatial segregation between BVOC and NOx emissions. This segregation implies that RONO2 production will remain a minor sink for NOx in the Southeast US in the future even as NOx emissions continue to decline.

SUBMITTER: Fisher JA 

PROVIDER: S-EPMC5906813 | biostudies-literature | 2016

REPOSITORIES: biostudies-literature

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Organic nitrate chemistry and its implications for nitrogen budgets in an isoprene- and monoterpene-rich atmosphere: constraints from aircraft (SEAC<sup>4</sup>RS) and ground-based (SOAS) observations in the Southeast US.

Fisher J A JA   Jacob D J DJ   Travis K R KR   Kim P S PS   Marais E A EA   Miller C Chan CC   Yu K K   Zhu L L   Yantosca R M RM   Sulprizio M P MP   Mao J J   Wennberg P O PO   Crounse J D JD   Teng A P AP   Nguyen T B TB   St Clair J M JM   Cohen R C RC   Romer P P   Nault B A BA   Wooldridge P J PJ   Jimenez J L JL   Campuzano-Jost P P   Day D A DA   Hu W W   Shepson P B PB   Xiong F F   Blake D R DR   Goldstein A H AH   Misztal P K PK   Hanisco T F TF   Wolfe G M GM   Ryerson T B TB   Wisthaler A A   Mikoviny T T  

Atmospheric chemistry and physics 20160517 9


Formation of organic nitrates (RONO<sub>2</sub>) during oxidation of biogenic volatile organic compounds (BVOCs: isoprene, monoterpenes) is a significant loss pathway for atmospheric nitrogen oxide radicals (NO<sub>x</sub>), but the chemistry of RONO<sub>2</sub> formation and degradation remains uncertain. Here we implement a new BVOC oxidation mechanism (including updated isoprene chemistry, new monoterpene chemistry, and particle uptake of RONO<sub>2</sub>) in the GEOS-Chem global chemical tra  ...[more]

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