L. Magi et al., INVESTIGATION OF THE UPTAKE RATE OF OZONE AND METHYL HYDROPEROXIDE BYWATER SURFACES, The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 101(27), 1997, pp. 4943-4949
The uptake kinetics of ozone (O-3) and methyl hydroperoxide (CH3OOH, M
HP) by aqueous solutions were studied as a function of temperature usi
ng the droplet train technique combined with mass spectrometry detecti
on. The uptake of ozone by pure water was found to be too small to be
directly measured. Using NaI as a scavenger increased the uptake coeff
icient gamma from below the detection limit to a range from 0.0037 to
0.0116 for I- activities in the range from 0.3615 to 2.889 at 282 K. F
rom these experiments, we estimated the second-order rate constant for
the reaction O-3 + I- --> products to be in the range 3.2 x 10(8) to
2.4 x 10(9) M-1 s(-1) for temperature between 275 and 293 K. The activ
ation parameters for this reaction were also estimated. For methyl hyd
roperoxide, the uptake rate on pure water was fast enough to be direct
ly measured. According to the physicochemical properties of this hydro
peroxide, the uptake was mainly due to the diffusion and accommodation
processes. It was therefore possible to measure its mass accommodatio
n coefficient alpha as a function of temperature. The observed values
are in the range 0.92 x 10(-2) to 2.08 x 10(-2) for temperature betwee
n 281 and 261 K. The activation parameters for the accommodation were
also determined.