The photoinduced decomposition of trichloroethylene adsorbed on Ca-montmori
llonite by long-wavelength UV irradiation has been studied in a quartz tube
open to air or through which air or oxygen is passed. Solid-sample and liq
uid-solution NMR techniques were used to identify apparent products or inte
rmediates of the photodecomposition. Dichloroacetic acid was identified as
a major organic product/intermediate; substantial amounts of pentachloroeth
ane and trichloroacetic acid were also identified. The formation of CO2 was
characterized quantitatively by wet chemical analysis. About 40% and 57%,
respectively, of the total carbon of trichloroethylene was converted to car
bon dioxide in air and O-2 environments over a period of 16 days; Phosgene
and HCl were also defected. The photodecomposition of trichloroethylene ads
orbed on whole soil, on Zn2+-exchanged and Cu2+-exchanged montmorillonites,
on kaolinite, and on silica gel was also examined in less detail; qualitat
ively, the conversion of trichloroethylene to dichloroacetic acid in a 48-h
period occurred with the following order of decreasing efficiencies: Zn2+-
montmorillonite > silica gel > kaolinite > Ca2+-montmorillonite > whole soi
l > Cu2+-montmorillonite. These results show that the photoinducecl decompo
sition of adsorbed trichloroethylene occurs on a variety of adsorbents, gen
erating products and intermediates that are similar to what have been repor
ted previously for TiO2-based photodecomposition but with much longer time
scales. These conversions can, therefore, be expected to occur in sunlight
at the air-soil interface.