ABSTRACT

Since the advent of nuclear technology, the dissolution behavior of uranium oxides has been a matter of great practical importance in all stages of fuel production. In extractive metallurgy of uranium ores, acid and alkaline leaching in the presence of O2 and carbonate are procedures of widespread use. This chapter discusses that oxidative dissolution assisted by carbonate complexation of UO2+ is probably the most practical way to dissolve UO2. This oxide constitutes the basis of two common minerals, pichtblende and uraninite. Uranium mining raises concern about the possible contamination of aquatic systems by mine tailings and wastes; sound management therefore requires an adequate understanding of the mobilization of uranium, a process mediated by dissolution in mildly oxidic conditions. Oxidative dissolution is potentially a major source of error in the experimental attempts to measure the solubility of UO2 as a U(IV) concentration value.