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Kinetics and mechanisms of the reactions of OH with some oxygenated compounds of importance in tropospheric chemistry
Author(s) -
Saunders S. M.,
Baulch D. L.,
Cooke K. M.,
Pilling M. J.,
Smurthwaite P. I.
Publication year - 1994
Publication title -
international journal of chemical kinetics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.341
H-Index - 68
eISSN - 1097-4601
pISSN - 0538-8066
DOI - 10.1002/kin.550260112
Subject(s) - chemistry , torr , reaction rate constant , kinetics , ozone , photodissociation , troposphere , molecule , helium , atmosphere (unit) , total pressure , atmospheric pressure , chemical kinetics , analytical chemistry (journal) , photochemistry , thermodynamics , organic chemistry , meteorology , physics , quantum mechanics
The kinetics of the reactionshave been studied in a discharge flow system under pseudo‐first‐order conditions. The OH concentration was monitored by laser induced fluorescence and helium was used as the carrier gas. Values of k 1 = (8.1 ± 1.7) × 10 −13 , k 2 = (1.31 ± 0.26) × 10 −11 , k 3 = (2.6 ± 0.5) × 10 −11 , and k 4 = (2.5 ± 0.4) × 10 −11 cm 3 molecule −1 s −1 , at 298 K and 1 torr total pressure, were obtained. To validate the newly constructed system the rate constant for the reactionwas determined in a similar manner. The value of k 5 = (6.7 ± 0.9) × 10 −12 cm 3 molecule −1 s −1 at 298 K and 1 torr total pressure is in very good agreement with other literature values. The mechanisms for the atmospheric degradation of these compounds have been constructed to allow their incorporation in a photochemical trajectory computer model, to assess their impact on photochemical ozone creation in the troposphere. © 1994 John Wiley & Sons, Inc.