posted on 2013-09-03, 00:00authored byJosé M. Cerrato, Matthew
N. Ashner, Daniel S. Alessi, Juan S. Lezama-Pacheco, Rizlan Bernier-Latmani, John R. Bargar, Daniel E. Giammar
Aqueous
chemical extractions and X-ray absorption spectroscopy
(XAS) analyses were conducted to investigate the reactivity of chemogenic
uraninite, nanoparticulate biogenic uraninite, and biogenic monomeric
U(IV) species. The analyses were conducted in systems containing a
total U concentration that ranged from 1.48 to 2.10 mM. Less than
0.02% of the total U was released to solution in extractions that
targeted water-soluble and ion exchangeable fractions. Less than 5%
of the total U was solubilized via complexation with a 0.1 M solution
of NaF. Greater than 90% of the total U was extracted from biogenic
uraninite and monomeric U(IV) after 6 h of reaction in an oxidizing
solution of 50 mM K2S2O8. Additional
oxidation experiments with lower concentrations (2 mM and 10 mM) of
K2S2O8 and 8.2 mg L–1 dissolved oxygen suggested that monomeric U(IV) species are more
labile than biogenic uraninite; chemogenic uraninite was much less
susceptible to oxidation than either form of biogenic U(IV). These
results suggest that noncrystalline forms of U(IV) may be more labile
than uraninite in subsurface environments. This work helps fill critical
gaps in our understanding of the behavior of solid-associated U(IV)
species in bioremediated sites and natural uranium ore deposits.