U0 2 (s) / Salt brine / Redox conditions / Dissolution
SummaryThe dissolution of unirradiated U0 2 (s) in two different salt brines, a NaCl-brine and a MgCl 2 -brine, under different redox conditions has been modeled.The experimental data have been modeled taking into account two different processes: (1) an initial dissolution due to the existence of an oxidized layer initially present on the U0 2 (s) surface and (2) the evolution of the uranium concentration in solution to reach the solubility of the thermodynamically stable solid phase. The good agreement between the model and the experimental data allows the establishment of an U0 2 (s) dissolution mechanism under the experimental conditions.Results have shown that the long-term dissolution rate depends on the square root of the oxygen partial pressure. This fractional dependence has been attributed to the fact that the rate limiting step is the adsorption of the oxygen on the surface of the solid and the diffusion of this oxygen through the U0 2 (s) lattice.