Reactions of Cl atoms with CH3I, C2H5I, 1-C3H7I, 2-C3H7I and CF3I: kinetics and atmospheric relevance

Citation
Esn. Cotter et al., Reactions of Cl atoms with CH3I, C2H5I, 1-C3H7I, 2-C3H7I and CF3I: kinetics and atmospheric relevance, PHYS CHEM P, 3(3), 2001, pp. 402-408
Citations number
53
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
PHYSICAL CHEMISTRY CHEMICAL PHYSICS
ISSN journal
14639076 → ACNP
Volume
3
Issue
3
Year of publication
2001
Pages
402 - 408
Database
ISI
SICI code
1463-9076(2001)3:3<402:ROCAWC>2.0.ZU;2-#
Abstract
The kinetics of the reactions [GRAPHICS] were studied at T = 298 K using a fast-flow discharge system with resonance -fluorescence detection of Cl atoms. The rate coefficients were found to be pressure-independent over the range 1.5-12 Torr, and were k(1) = (1.51 +/- 0.15) x 10(-12) cm(3) molecule(-1) s(-1), k(2) = (16.0 +/- 1.7) x 10(-12) cm(3) molecule(-1) s(-1), k(3) = (66.5 +/- 7.5) x 10(-12) cm(3) molecule(-1 ) s(-1), k(4) = (46.8 +/- 4.9) x 10(-12) cm(3) molecule(-1) s(-1) and k(5) = (0.85 +/- 0.09) x 10(-12) cm(3) molecule(-1) s(-1). The rates of reaction of these alkyl iodides with Cl atoms in the marine boundary layer were com pared with the rates of their photolysis and their reaction with OH. For ea rly morning conditions, it is shown that reaction with Cl atoms can compete with photolysis and dominate over reaction with OH, if Cl atom concentrati ons are about 1 x 10(5) molecule cm(-3). Atomic iodine may be released foll owing reaction of Cl with the alkyl iodides; this atomic I can participate in catalytic destruction of ozone in the marine boundary layer.