2
54
GELIS et al.
than the rate of the oxidation of Се(III) to Ce(IV) with
ozone. This is also confirmed by the fact that an in-
crease in the ozone concentration in OOM leads to a
considerable increase in the steady-state concentration
of Се(IV) and, correspondingly, to an increase in the
UO dissolution rate (Table 1).
2
Thus, in the presence of Се(IV), the UO dissolu-
2
tion rate increases further (by a factor of more than 3).
This acceleration is apparently due to the fact that
Се(IV) ions, when adsorbed on the UO surface, react
2
with UO faster than neutral О molecules do, and the
2
3
Fig. 4. Kinetic curves of the oxidative dissolution of a UO
pellet in 1.0 M HNO in the presence (or in the absence) of
.023 M Се(III) at various О concentrations in the ozone–
oxygen mixture: (1) without Се and О ; (2) without Се,
2
Сe(III) ions formed in the process are sufficiently rap-
idly oxidized both with ozone and with products of its
spontaneous decomposition.
3
0
3
3
–
3
–3
1
80 mg dm
O ; (3) in the presence of Ce, 30 mg dm O ;
3
3
The results of our study furnished the first experi-
mental confirmation for the fact that the rate of the
Сe(IV) accumulation and the rate of the dissolution of
–3
and (4) in the presence of Ce, 180 mg dm
3
O .
highly calcined UO in nitric acid solutions under the
2
conditions of oxidation of Се(III) to Се(IV) with ozone
strongly depend on the content of О in OOM. With
3
–
1
OOM containing 170–180 mg l О , oxidation of
3
Ce(III) to Ce(IV) in the course of ozonation of nitric
acid solutions of Ce(III) occurs with the formation of
approximately 2.0 mol of Се(IV) per mole of the con-
sumed ozone, i.e., in accordance with Eq. (1). This
result can be used when developing procedures for
intensifying the dissolution of PuO -containing materi-
2
als, e.g., of high-level PuO .
2
REFERENCES
Fig. 5. Curves of Ce(IV) accumulation in solutions at vari-
–
3
ous ozone concentrations in OOM, mg dm : (1) 170,
2) 170 + UO , (3) 30, and (4) 30 + UO
1
2
. Clark, D.L., Hecker, S.S., Jarvinen, G.D., and
Neu, M.P., The Chemistry of the Actinide and Trans-
actinide Elements, Morss, L.R., Edelstein, N.M., and
Fuger, J., Eds., Dordrecht: Springer, 2006, vol. 3, ch. 7,
p. 1118.
. Ryan, J.L., Bray, L.A., Wheelwright, E.J., and
Bryan, G.H., Catalyzed Electrolytic Plutonium Oxide
Dissolution (CEPOD): The Past Seventeen Years and
Future Potential. PNL-SA-18018; CONF-900846-5, 1990.
(
2
2
.
In the presence of Ce(IV) ions, the UO dissolution
2
rate increases. This trend is the most pronounced at a
high ozone concentration in OOM. In this connection,
it was interesting to determine how the steady-state
concentration of Се(IV) in the solution varies in the
course of UO dissolution and how this parameter de-
3. Bourges, J., Madic, C., Koehly, G., and Lecomte, M.,
2
J. Less-Common Met., 1986, vol. 122, no. 2, pp. 303–
pends on the ozone concentration in OOM.
3
07.
Comparison of the kinetics curves of the Се(IV)
4
. Runde, W.H. and Shultz, W.W., The Chemistry of Acti-
nide Elements, Morss, L., Edelstein, N., Fuger, J., and
Katz, J.J., Eds., New York: Springer, 2005, vol. 2,
p. 1326.
. Trushima, S., Nagasaki, S., and Suzuki, A., Sep. Sci.
Technol., 1996, vol. 31, no. 17, pp. 2443–2453.
. Ivanov, Yu.E. and Nikitina, G.P., Radiokhimiya, 1995,
vol. 37, no. 3, pp. 214–220.
accumulation in the course of UO dissolution with the
2
results of blank experiments (Fig. 5) showed that the
attained concentrations of Се(IV) were independent of
whether the process was performed simultaneously
5
6
with UO dissolution or without it (curves 1, 2 and 3,
2
4
). This means that the rate of the heterogeneous reac-
tion of U(IV) oxidation to U(VI) is considerably lower
RADIOCHEMISTRY Vol. 53 No. 3 2011