Va. Volkovich et al., Chemical solubility of alkali metal uranate(VI) species in molten carbonates under basic and acidic conditions, PHYS CHEM P, 2(13), 2000, pp. 3029-3035
A detailed investigation of the dissolution of alkali metal uranates in car
bonate melts under the influence of CO2 and O-2 partial pressures has been
performed between 450 and 800 degrees C. At low temperatures or high CO2 pr
essure an acidic melt is formed. Acidic dissolution of uranates releases ox
ide ions and the possible dissolution routes of mono- and diuranates are di
scussed. At high temperatures carbonates begin to decompose, lose CO2, and
become basic melts. Under these conditions, basic dissolution of uranates o
ccurs and again the possible routes and products are discussed. Oxygen part
ial pressure influences uranate dissolution due to the formation of peroxyc
arbonate complexes. Under acidic conditions and using pure O-2 under pressu
re a maximum solubility of K2UO4 of ca. 37 mol ppm in (Li-Na-K)(2)CO3 eutec
tic was evaluated. This system, when under CO2 and below 600 degrees C, did
not produce the expected yellow coloured (quenched) melts from the dissolu
tion of uranates, but gave grey melts that became yellow only on heating ab
ove 600 degrees C. The reproducible grey colour is due to a minor contribut
ion from intervalence bands resulting from the formation of very low concen
trations of oxygen-deficient polyuranates under these conditions.