<p>In alkaline and saline solutions, uranium
VI (U<sup>VI</sup>)<sup> </sup>forms uranyl salts, limiting its mobility in leachates
released from nuclear waste repositories into groundwater. However, recent experimental
and computational work suggested that natural organic molecules widely present
in groundwater such as siderophores could potentially prevent solid
precipitation because of the formation of stable UVI-siderophore complexes. It
is important we assess the impact of siderophores on aqueous U<sup>VI</sup>
chemistry as they could mobilise U<sup>VI
</sup>from contaminated land and radioactive waste storage and disposal sites. Here we test this hypothesis by combining for
the first time experimental studies on uranium precipitation in alkaline pH in the presence of desferrioxamine
B (DFOB) and electron structure method calculation of uranyl – hydroxamate
complexes to assess their stability. Stirred batch experiments containing 0 to 420
µM DFOB, 42 µM U<sup>VI</sup> and 0.1 M NaCl were
conducted at pH 11.5. DFT was employed to explore the relative stability of
different U<sup>VI</sup>-hydroxamate complexes, representative of the local
binding mode of DFOB. During the stirred batch experiments, 5%, 11-12%, 41-53%,
95-96% and 100% of U<sup>VI</sup> passes through the filter membranes (0.2-1 µm pore diameter) after 24 hours when
0, 4.2, 42, 130 and 420 µM DFOB
was added to solution. The DFT results suggest one hydroxamate functional group
is most likely to complex with U<sup>VI</sup> with ∆<sub>r</sub>G calculated as
+3 kJ/mol and -9 kJ/mol for [UO<sub>2</sub>(OH)<sub>3</sub>(L<sub>mono</sub>)]<sup>2-
</sup>and [UO<sub>2</sub>(OH)<sub>2</sub>(L)]<sup>-</sup> respectively.
Conversion of the experimentally derived log β (-1.2 ± 0.3) through the equation ∆<sub>r</sub>G = -2.303RTlogβ provides
∆<sub>r</sub>G of +7 kJ/mol, similar to the ∆<sub>r</sub>G of these two
complexes. The results of our study confirm that U<sup>VI</sup> precipitation
could be hindered by the formation of a DFOB complex with U<sup>VI</sup> complexation
through a single hydroxamate functional group as a likely mechanism. These
results highlight the mobilising effect siderophores have on U<sup>VI</sup>
from contaminant sources and need to be incorporated in environmental risk
assessment studies.</p>