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
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.