Sa. Carl et al., RATE-CONSTANT AND MECHANISM OF THE REACTION BETWEEN CL AND CH3OCL AT 295 K, Journal of physical chemistry, 100(43), 1996, pp. 17191-17201
The reaction between Cl atoms and CH3OCl was investigated at 295 K in
both air and N-2 bath gases at total pressures between 100 and 750 Tor
r by the relative rate method. The rate constant of the title reaction
was found to be a factor 1.07 +/- 0.02 (2 sigma) greater than that of
Cl + C2H6 at room temperature and independent of pressure between 100
and 750 Torr, This yields a rate constant of (6.1 +/- 0.6) x 10(-11)
cm(3) molecule(-1) s(-1). The products of the reaction were detected b
y FTIR and UV absorption spectroscopy. Analysis of Cl-2 s and HCl prod
ucts allowed branching ratios of 0.2 +/- 0.1 for HCl + CH2OCl formatio
n and 0.8 +/- 0.2 for Cl-2 + CH3O formation to be determined. The high
rate constant implies that reaction with Cl atoms is an important los
s process for CH3OCl in the polar stratosphere.