The solubility behavior of uranium dioxide was studied under oxidizing cond
itions in the Belgian Boom clay water at 25 degreesC up to 323 days. X-ray
photoelectron spectroscopy analyses reveal that both U(VI) and U(IV) oxidat
ion states are present in the altered layer. The U(VI)/U(IV) ratio in this
altered layer increases up to 43 days and then remains constant throughout
the whole test. In the leachate the uranium concentration also increases up
to 43 days and then stabilizes. It is rather unlikely that the altered lay
er formed on the surface controls thermodynamically the uranium solubility.
It is rather probable that the system has reached a pseudo-equilibrium gov
erned by kinetics. (C) 2000 Elsevier Science B.V. All rights reserved.