Atmospheric loss of nitrous oxide (NO) is not influenced by its potential reactions with OH and NO radicals

The rate coefficient for the possible reaction of OH radical with N 2 O was determined to be k 1 < 1 × 10 −17 cm 3 molecule −1 s −1 between 253 and 372 K using pulsed laser photolysis to generate OH radicals and pulsed laser induced fluorescence to detect them. The rate coefficient for the reacti...

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Published inPhysical chemistry chemical physics : PCCP Vol. 21; no. 44; pp. 24592 - 246
Main Authors Ravishankara, A. R, Pele, Anne-Laure, Zhou, Li, Ren, Yangang, Zogka, Antonia, Daële, Véronique, Idir, Mahmoud, Brown, Steven S, Romanias, Manolis N, Mellouki, Abdelwahid
Format Journal Article
Published 13.11.2019
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Abstract The rate coefficient for the possible reaction of OH radical with N 2 O was determined to be k 1 < 1 × 10 −17 cm 3 molecule −1 s −1 between 253 and 372 K using pulsed laser photolysis to generate OH radicals and pulsed laser induced fluorescence to detect them. The rate coefficient for the reaction of NO 3 radical with N 2 O was measured to be k 2 < 5 × 10 −20 cm 3 molecule −1 s −1 at 298 K using a direct method that involves a large reaction chamber equipped with cavity ring down spectroscopic detection of NO 3 and N 2 O 5 . Various tests were carried out ensure the accuracy of our measurements. Based on our measured upper limits, we suggest that these two reactions alter the atmospheric lifetime of N 2 O of ∼120 years by less than 4%. The rate coefficient for the possible reaction of OH and NO 3 radical with N 2 O are shown to be, respectively, <1 × 10 −17 and <5 × 10 −20 cm 3 molecule −1 s −1 . They are too low to contribute significantly to the atmospheric removal of N 2 O.
AbstractList The rate coefficient for the possible reaction of OH radical with N 2 O was determined to be k 1 < 1 × 10 −17 cm 3 molecule −1 s −1 between 253 and 372 K using pulsed laser photolysis to generate OH radicals and pulsed laser induced fluorescence to detect them. The rate coefficient for the reaction of NO 3 radical with N 2 O was measured to be k 2 < 5 × 10 −20 cm 3 molecule −1 s −1 at 298 K using a direct method that involves a large reaction chamber equipped with cavity ring down spectroscopic detection of NO 3 and N 2 O 5 . Various tests were carried out ensure the accuracy of our measurements. Based on our measured upper limits, we suggest that these two reactions alter the atmospheric lifetime of N 2 O of ∼120 years by less than 4%. The rate coefficient for the possible reaction of OH and NO 3 radical with N 2 O are shown to be, respectively, <1 × 10 −17 and <5 × 10 −20 cm 3 molecule −1 s −1 . They are too low to contribute significantly to the atmospheric removal of N 2 O.
Author Ravishankara, A. R
Idir, Mahmoud
Romanias, Manolis N
Zhou, Li
Zogka, Antonia
Mellouki, Abdelwahid
Daële, Véronique
Ren, Yangang
Pele, Anne-Laure
Brown, Steven S
AuthorAffiliation Univ. Lille
Earth System Research Laboratory
Colorado State University
National Oceanic and Atmospheric Administration
Aérothermique
Department of Chemistry
CNRS
Chemical Sciences Division
IMT Lille Douai
Institut de Combustion
Réactivité et Environnement/OSUC
Departments of Chemistry and Atmospheric Science
Le Studium Loire Valley Institute for Advanced Studies
University of Colorado
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Title Atmospheric loss of nitrous oxide (NO) is not influenced by its potential reactions with OH and NO radicals
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