Deposition of ozone with either 2-iodopropane,
pentafluoroiodoethane, 1,1,1-trifluoroiodoethane, 1,1,2,2-tetrafluoroiodoethane, or 1,1,1,2-tetrafluoroiodoethane, in an argon
matrix at 14 K has been shown by FTIR
spectroscopy to lead to the formation of a molecular complex.
Irradiation of such complexes with near-infrared radiation led to the formation of the corresponding
iodoso-species (Z−IO). Radiation of wavelengths
> 410 nm produced bands typical of iodyl-species
(Z−IO2), while subsequent photolysis with UV−vis (λ
>
350 nm) radiation led to the development of bands attributed to
hypoiodo-species (Z−OI) and to carbonyl
complexes (carbonyl···XI, where X = H or F). Further
photolysis using Pyrex- (λ > 290 nm) and quartz-
(λ > 240 nm) filtered radiation increased the yield of the carbonyl
complexes, which were the final products
to be detected in the reaction series of each precursor with ozone.
Sample annealing confirmed that the
carbonyl complexes existed in two geometric arrangements, a
molecular-pair type and a head-to-tail dipole−dipole type. In a similar study of each precursor deposited in a
solid oxygen matrix the carbonyl complexes
were the only species that could be identified. Thus by studying
the reactions of ozone with these iodine-containing compounds it has been possible to extend the number of known
species having I−O
x
bonds, to
detect a number of carbonyl···XI complexes (X = H or F),
and to clarify the mechanisms of the reactions.