The solubility-product constant log K-sp(o)([UO22+](2)[SiO2]/[H+](4))
of uranyl orthosilicate ([UO2]2SiO4 . 2H(2)O) has been determined at p
H 3 and 25 degrees C in air and in N-2-atmosphere beginning from under
saturation conditions. The value derived under N-2-atmosphere was 6.03
+/-0.45 and in air 6.15+/-0.53 at infinite dilution. The experiments w
ere carried out at 25 degrees C in 0.1 M NaClO4 solution and at a pH r
anging from 3 to 9. Most solutions reached steady-state concentrations
after about 40 days. X-ray powder diffraction (XRD) measurements of t
he solid residues at steady-state showed that (UO2)(2)SiO4 . 2H(2)O al
one was the solubility-controlling solid. The results indicate that th
e solubility of uranyl orthosilicate depends on pH. It exhibits a mini
mum at a pH from 6 to 7. The observed concentration minimum is more pr
onounced in the air experiments than in the ones under N-2-atmosphere.
The results allow for a source term evaluation for uranyl orthosilica
te in natural systems.