The kinetics of the simplest Criegee intermediate (CH2OO) reaction with water vapor was revisited. By improving
the signal-to-noise
ratio and the precision of water concentration, we found that the
kinetics of CH2OO involves not only two water molecules
but also one and three water molecules. Our experimental results suggest
that the decay of CH2OO can be described as d[CH2OO]/dt = −k
obs[CH2OO]; k
obs = k
0 + k
1[water] + k
2[water]2 + k
3[water]3; k
1 = (4.22 ± 0.48) ×
10–16 cm3 s–1, k
2 = (10.66 ± 0.83) × 10–33 cm6 s–1, k
3 = (1.48 ± 0.17) × 10–50 cm9 s–1 at 298 K and 300 Torr with the respective
Arrhenius activation energies of E
a1 =
1.8 ± 1.1 kcal mol–1, E
a2 = −11.1 ± 2.1 kcal mol–1, E
a3 = −17.4 ± 3.9 kcal mol–1. The contribution of the k
3[water]3 term becomes less significant at higher temperatures around
345 K, but it is not ignorable at 298 K and lower temperatures. By
quantifying the concentrations of H2O and D2O with a Coriolis-type direct mass flow sensor, the kinetic isotope
effect (KIE) was investigated at 298 K and 300 Torr and KIE(k
1) = k
1(H2O)/k
1(D2O) = 1.30 ± 0.32;
similarly, KIE(k
2) = 2.25 ± 0.44
and KIE(k
3) = 0.99 ± 0.13. These
mild KIE values are consistent with theoretical calculations based
on the variational transition state theory, confirming that the title
reaction has a broad and low barrier, and the reaction coordinate
involves not only the motion of a hydrogen atom but also that of an
oxygen atom. Comparing the results recorded under 300 Torr (N2 buffer gas) with those under 600 Torr, a weak pressure effect
of k
3 was found. From quantum chemistry
calculations, we found that the CH2OO + 3H2O
reaction is dominated by the reaction pathways involving a ring structure
consisting of two water molecules, which facilitate the hydrogen atom
transfer, while the third water molecule is hydrogen-bonded outside
the ring. Furthermore, analysis based on dipole capture rates showed
that the CH2OO(H2O) + (H2O)2 and CH2OO(H2O)2 + H2O pathways will dominate in the three water reaction.