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Upper limits for the gas‐phase reaction of H 2 O 2 with O 3 and NO. Atmospheric implications
Author(s) -
Wallington T. J.,
Jucks K. W.,
Tyndall G. S.
Publication year - 1998
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/(sici)1097-4601(1998)30:10<707::aid-kin2>3.0.co;2-z
Subject(s) - chemistry , gas phase , phase (matter) , atmospheric chemistry , ozone , atmospheric sciences , organic chemistry , geology
Abstract Upper limits of 4×10 −20 and 7×10 −20 cm 3 molecule −1 s −1 were established for the gas‐phase reactions of H 2 O 2 with O 3 and NO, respectively. These reactions are too slow to explain features observed in the atmospheric vertical profile of H 2 O 2 . © 1998 John Wiley & Sons, Inc. Int J Chem Kinet: 30: 707–709, 1998