A determination of the rate constant for the reaction of HOCL with O-atoms at room temperature

A discharge fast flow system with mass spectrometric detection was used to determine the rate constant of the title reaction to be k(1) = (1.3±0.2)×10−13 cm3 molecule−1 s−1. This experimental value is roughly a factor of 20 higher than previously recommended. It is suggested that the title reaction...

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Veröffentlicht in:Geophysical research letters 1992-10, Vol.19 (19), p.1935-1937
Hauptverfasser: Vogt, Rainer, Schindler, Ralph N.
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container_end_page 1937
container_issue 19
container_start_page 1935
container_title Geophysical research letters
container_volume 19
creator Vogt, Rainer
Schindler, Ralph N.
description A discharge fast flow system with mass spectrometric detection was used to determine the rate constant of the title reaction to be k(1) = (1.3±0.2)×10−13 cm3 molecule−1 s−1. This experimental value is roughly a factor of 20 higher than previously recommended. It is suggested that the title reaction should be considered as a removal process in modeling stratospheric HOCl.
doi_str_mv 10.1029/92GL02100
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source Wiley Online Library Journals Frontfile Complete
subjects Atmospheric composition. Chemical and photochemical reactions
Earth, ocean, space
Exact sciences and technology
External geophysics
Physics of the high neutral atmosphere
title A determination of the rate constant for the reaction of HOCL with O-atoms at room temperature
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