Uranium is a chemically toxic and
radioactive heavy metal. Depleted
uranium (DU) is the byproduct of the uranium enrichment process, with
a majority of U as uranium-238, and a lower content of the fissile
isotope uranium-235 than natural uranium. Uranium-235 is mainly used
in nuclear reactors and in the manufacture of nuclear weapons. Exposure
is likely to have an impact on humans or the ecosystem where military
operations have used DU. Yuma Proving Ground in Arizona, USA has been
using depleted uranium ballistics for 36 years. At a contaminated
site in the Proving Grounds, soil samples were collected from the
flat, open field and lower elevated trenches that typically collect
summer runoff. Spatial distribution and fractionation of uranium in
the fields were analyzed with total acid digestion and selective sequential
dissolution with eight operationally defined solid-phase fractions.
In addition to uranium, other trace elements (As, Ba, Co, Cr, Cu,
Hg, Mo, Nb, Pd, Pb, V, Zn, Zr) were also assessed. Results show that
the trench area in the testing site had a higher accumulation of total
U (12.4%) compared to the open-field soil with 279 mg/kg U. Among
the eight solid-phase components in the open-field samples, U demonstrated
stronger affinities for the amorphous iron-oxide bound, followed by
the carbonate bound, and the residual fractions. However, U in the
trench area had a stronger binding to the easily reducible oxide bound
fraction, followed by the carbonate-bound and amorphous iron-oxide-bound
fractions. Among other trace elements, Nb, As, and Zr exhibited the
strongest correlations with U distribution among solid-phase components.
This study indicates a significant spatial variation of U distribution
in the shooting range site. Fe/Mn oxides and carbonate were the major
solid-phase components for binding U in the weapon test site.