ATMOSPHERIC CHEMISTRY OF CH2BR2 - RATE COEFFICIENTS FOR ITS REACTION WITH CL ATOMS AND OH AND THE CHEMISTRY OF THE CHBR2O RADICAL

Citation
Jj. Orlando et al., ATMOSPHERIC CHEMISTRY OF CH2BR2 - RATE COEFFICIENTS FOR ITS REACTION WITH CL ATOMS AND OH AND THE CHEMISTRY OF THE CHBR2O RADICAL, International journal of chemical kinetics, 28(6), 1996, pp. 433-442
Citations number
40
Categorie Soggetti
Chemistry Physical
ISSN journal
05388066
Volume
28
Issue
6
Year of publication
1996
Pages
433 - 442
Database
ISI
SICI code
0538-8066(1996)28:6<433:ACOC-R>2.0.ZU;2-V
Abstract
Rate coefficients for the reaction of OH radicals and Cl atoms with di bromomethane, OH + CH2Br2 --> CHBr2 + H2O (1) and Cl + CH2Br2 --> CHBr 2 + HCl (3), and for the reaction of Cl atoms with methyl bromide, Cl + CH3Br --> HCl + CH2Br (4), have been obtained using relative rate te chniques. At 298 K, the value of k(1) was determined to be (1.2 +/- 0. 3) x 10(-13) cm(3) molec(-1) s(-1). The rate coefficients k(3) and k(4 ) were determined at a series of temperatures ranging from 228 K to 29 6 K and combined with the measurements of Gierczak et al., yielding th e following Arrhenius expressions for k(3) and k(4); k(3) = (6.35 +/- 0.6) x 10(-12) exp(-807 +/- 50/T) cm(3) molec(-1) s(-1) and k(4) = (1. 49 +/- 0.2) x 10(-11) exp(-1056 +/- 50/T) cm(3) molec(-1) s(-1). In ad dition, the Cl atom initiated oxidation mechanism of CH2Br2 in air has been studied at 298 K. The products observed were HC(O)Br and small a mounts of CO. The dominant atmospheric fate of the alkoxy radical, CHB r2O, is elimination of a Br atom, which occurs at the rate estimated t o be greater than 4 x 10(6) s(-1) in 700 torr of O-2 at 298 K. (C) 199 6 John Wiley & Sons, Inc.