Plutonium (Pu) has
been released to the environment worldwide,
including approximately 1.85 × 1015 Bq (200 kg) of
Pu from process waste solutions to unconfined soil structures at the
Hanford Site in Washington State. The subsurface mobility of Pu is
influenced by complex interactions with sediments, groundwater, and
any co-contaminants within the waste stream. Previous investigations
at Hanford have shown that Pu exists as discrete PuO2 particles
forming before or after disposal, as secondary solid phases formed
from waste interactions with sediments as adsorbed/incorporated species,
and/or as dissolved species. In this research, new evidence is presented
for the existence of PuO2, PuO2-Bi2O3 composites, and particles from burnt Pu metal in near-surface
sediments where Pu-laden acidic process waste was disposed to sediments.
Pu and americium (Am) L
3 X-ray absorption
spectroscopy and density functional theory suggest that, in larger,
more crystalline PuO2 particles, Am formed from radioactive
decay is retained in the PuIVO2 structure as
AmIV. The Pu and Am that were disposed of in an acidic
waste stream have since migrated deeper into the subsurface with detection
to at least 37 meters below ground surface. In contrast, Pu deposited
near the ground surface from neutral pH waste is found to be homogeneously
distributed and relatively immobile. Groundwater extractions performed
on contaminated sediments indicate that both Pu and Am are recalcitrant,
with Am being fractionally less extractable than Pu on a molar basis.
These results suggest that the more mobile fraction of Am has migrated
from the near-surface and may be present in the deeper sediments as
a different phase than Pu. From these results, it is suggested that
Pu and Am deposited from acidic wastes were initially mobile and became
significantly less mobile as wastes were neutralized within the soil
profile.