In the United Kingdom, decommissioning
of legacy spent fuel storage
facilities involves the retrieval of radioactive sludges that have
formed as a result of corrosion of Magnox nuclear fuel. Retrieval
of sludges may re-suspend a colloidal fraction of the sludge, thereby
potentially enhancing the mobility of radionuclides including uranium.
The colloidal properties of the layered double hydroxide (LDH) phase
hydrotalcite, a key product of Magnox fuel corrosion, and its interactions
with U(VI) are of interest. This is because colloidal hydrotalcite
is a potential transport vector for U(VI) under the neutral-to-alkaline
conditions characteristic of the legacy storage facilities and other
nuclear decommissioning scenarios. Here, a multi-technique approach
was used to investigate the colloidal stability of hydrotalcite and
the U(VI) sorption mechanism(s) across pH 7–11.5 and with variable
U(VI) surface loadings (0.01–1 wt %). Overall, hydrotalcite
was found to form stable colloidal suspensions between pH 7 and 11.5,
with some evidence for Mg
2+
leaching from hydrotalcite
colloids at pH ≤ 9. For systems with U present, >98% of
U(VI)
was removed from the solution in the presence of hydrotalcite, regardless
of pH and U loading, although the sorption mode was affected by both
pH and U concentrations. Under alkaline conditions, U(VI) surface
precipitates formed on the colloidal hydrotalcite nanoparticle surface.
Under more circumneutral conditions, Mg
2+
leaching from
hydrotalcite and more facile exchange of interlayer carbonate with
the surrounding solution led to the formation of uranyl carbonate
species (e.g., Mg(UO
2
(CO
3
)
3
)
2–
(aq)
). Both X-ray absorption spectroscopy
(XAS) and luminescence analysis confirmed that these negatively charged
species sorbed as both outer- and inner-sphere tertiary complexes
on the hydrotalcite surface. These results demonstrate that hydrotalcite
can form pseudo-colloids with U(VI) under a wide range of pH conditions
and have clear implications for understanding the uranium behavior
in environments where hydrotalcite and other LDHs may be present.