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
The kinetics of the reactions
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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.