The
role of the water molecule in the atmospheric reaction between
CH3COCH3 and Cl atoms was investigated at the
theoretical level of CCSD(T)/aug-cc-pVTZ//BHandHLYP/aug-cc-pVDZ. The
reaction between acetone and Cl atoms proceeds through three paths:
an H-abstraction reaction, a −CH3 abstraction reaction,
and an addition/elimination reaction by Cl, leading to the formation
of CH3COCH2 + HCl (+H2O), CH3CO + CH3Cl (+H2O), and CH3COCl + CH3 (+H2O), respectively. The formation
pathway of CH3COCH2 + HCl in the three paths
occupies a dominant position, with a rate constant of 1.08 ×
10–12 cm3 molecule–1 s–1. However, water-assisted CH3COCH3 + Cl reactions become more complex, proceeding through 10
different paths. At 298 K, the effective rate constant for CH3COCH2 + HCl + H2O formation is 8.46
× 10–15 cm3 molecule–1 s–1, and the effective rate constant decreases
by 3–4 orders of magnitudes in the temperature range of 216.69–298.15
K. Therefore, it is concluded that water exerts a hindering effect
on the CH3COCH3 + Cl + H2O reaction
under atmospheric conditions, but it is not enough to change the dominant
position of the CH3COCH3 + Cl reaction under
anhydrous conditions.