1704 Bull. Chem. Soc. Jpn., 75, No. 8 (2002)
Flash Photolysis and Pulse Radiolysis of CF2Br2
However, reaction (18) cannot explain the formation of Br− in
steady state photolysis, where the probability of its occurrence
would be practically zero. Also, a biphotonic process involv-
ing the photoionization of CF2Br2 molecule is not considered
for the same reason. A plausible mechanism can be as follows:
tion about the absorption spectrum and the reactivity of the pri-
mary product CF2Br· radical.
It has been estimated that on a per atom basis, bromine is
~50 times more efficient than chlorine in destroying atmo-
spheric ozone.32 This efficiency results from the fact that near-
ly 50% of the available bromine in the stratosphere exists in
the reactive form (Br· and BrO·), whereas only a percent or so
of stratospheric chlorine exists as ClO·. In view of this, it is
interesting to examine the atmospheric implications of our re-
sults. A higher value of its solubility compared to that of most
other halons and CFCs implies a reduced tropospheric lifetime
for CF2Br2 due to uptake by water in the oceans, rivers, lakes,
etc. However, detail information on the marine chemistry of
CF2Br2 is required to understand whether the oceans act as a
sink or reservoir for this molecule. In addition, an enhance-
ment in the solubility of CF2Br2 in the condensed aqueous
phase at the lower temperatures encountered in the strato-
sphere may be significant. This possibility coupled with the
fact that the UV photochemistry of CF2Br2 in the aqueous
phase is also different from that in the gas phase, partly leading
to the formation of Br− and H3O+ ions and hence to the miner-
alization of bromine, indicate that the findings of the present
work are likely to have an important impact on the atmospheric
modeling of CF2Br2 and on the depletion of ozone.
(CF2Br2)aq + hν → CF2Br· + Br·,
(19)
(20)
(CF2Br2)aq + hν → CF2BrOH + H3O+ + Br−,
where reactions (19) and (20) are two different primary photo-
chemical reactions which generate the reactants Br· and Br−
for reaction (14), and thus explain the intensity-square depen-
−
dence of the formation of Br2 . The photo-induced hydrolytic
reaction (20) accounts for the lowering of the pH as well as for
the formation of Br−. Further, reaction (19) represents a ho-
molytic cleavage (giving radicals), which is favored in the gas
phase as well as in non-polar solvents. Reaction (20) can be
considered to involve a heterolytic cleavage (giving cation and
anion), which is favored in polar solvents, like water, followed
by the reactions of ionic fragments with the solvent-molecules
available in the immediate vicinity, i.e.,
CF2Br2 + hν → CF2Br+ + Br−,
(20a)
(20b)
CF2Br+ + H2O → CF2BrOH + H+,
We thank Mr. Vijendra N. Rao and his colleagues for their
technical help in pulse radiolysis work.
H+ + nH2O → H3O+
Br− + nH2O → Br−
,
∆H = −11.3 eV (20c)
∆H = −3.6 eV (20d)
aq
,
aq
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tion between 225 and 275 nm (Fig. 4) is likely to have contri-
butions from more than one chemical species. Hence, we have
used the pulse radiolysis technique to obtain reliable informa-