Experiments have been carried out on the oxidation of the four chlorinated ethenes H2CCCl2, HClCCClH, HClCCCl2, and Cl2CCCl2. Reaction was initiated by continuous photolysis of Cl2, and product
yields were measured using Fourier transform infrared (FTIR) spectroscopy. In all cases, experiments were
performed at different concentrations of the chlorinated ethenes (down to 3 × 1013 molecule cm-3), Cl2 and
O2. In the cases of H2CCCl2 and HClCCCl2, the product yields were invariant with these changes, consistent
with them being determined by competitive unimolecular dissociations of the chlorinated alkoxy radical; that
is, H2ClCCCl2O (HCl2CCCl2O) (+M) → H2ClCCOCl (HCl2CCOCl) + Cl (+M) and H2ClCCCl2O (HCl2CCCl2O) (+M) → COCl2 + CH2Cl (CHCl2) (+M), and the subsequent formation of HCOCl and/or COCl2
from CH2Cl and CHCl2. In the case of HCl2CCHClO formed from HClCCClH, H atom abstraction by O2
is competitive with CCl and CC bond cleavage, so the yields depended on the concentration of O2. With
C2Cl4, the only products observed were CCl3COCl and COCl2, consistent with competitive dissociations of
perchloroethyl radicals: CCl3CCl2O (+M) → CCl3COCl + Cl (+M); CCl3CCl2O (+M) → COCl2 + CCl3
(+M). However, the relative yields of CCl3COCl and COCl2 were found to depend on the initial concentration
of C2Cl4 which is incompatible with the simple, and generally accepted, mechanism. To investigate this
unexpected result further, experiments were performed on pentachloroethane (C2Cl5H). Again, the product
yields depended on the initial concentration of the chlorinated compound. In addition, product yields from
C2Cl4 were measured using two different rates of photolysis of Cl2, at three temperatures, 298, 353, and 393
K, and in the presence of added NO and added HCl. Although the experimental results could be modeled
when bimolecular reactions of perchlorinated methoxy and ethoxy radicals with C2Cl4 and HCl were included
in the reaction mechanisms, the values of the rate constants which were needed seem unrealistically large if
the currently accepted rate for the unimolecular decomposition of CCl3CCl2O is correct. This observation on
C2Cl4 is important since it casts doubt on the current view of the oxidative chemistry of this compound,
which is released in significant amounts into the atmosphere.