Jf. Mccarthy et al., MOBILIZATION OF TRANSURANIC RADIONUCLIDES FROM DISPOSAL TRENCHES BY NATURAL ORGANIC-MATTER, Journal of contaminant hydrology, 30(1-2), 1998, pp. 49-77
Citations number
66
Categorie Soggetti
Water Resources","Environmental Sciences","Geosciences, Interdisciplinary
Transuranic (TRU) radionuclides in groundwater at the Oak Ridge Nation
al Laboratory migrate rapidly and with little retardation of the radio
nuclides over distances of 80 m. Several interacting hydrogeochemical
processes contribute to the observed releases of actinides (Cm-244 and
Am-241) from the shallow unlined disposal trenches, through the highl
y weathered, fractured shale (saprolite) and to the surface-water seep
s at White Oak Creek. Major releases are promoted when seasonal fluctu
ations in the water table permit groundwater to contact actinide-conta
minated waste. Local recharge of stormwater into the trenches appears
to permit minor releases, perhaps due to transient saturation within t
he trenches but above the local water table. Although the hydrogeology
of the site permits contact of the TRU waste with the groundwater, th
e expected inorganic species of the actinides should strongly adsorb t
o the layer silicates and mineral oxides of the shale saprolite, Yet t
he timing of the actinide releases relative to when rising groundwater
intercepts the trenches suggests that actinide transport is rapid, an
d the relative magnitude of peak actinide levels in wells near the tre
nches and at downgradient seeps suggests that then is very limited ret
ention of the actinides by the formation. Based on anion exchange chro
matography of the groundwater and geochemical modeling, the mobilizati
on and transport of the actinides is demonstrated to result from compl
exation of the actinides by natural organic matter (NOM). Storm events
contribute to mobilization by promoting hydrologic links between the
TRU waste and groundwater, and by increasing the concentration of NOM
in the mobile soil and groundwater. This study demonstrates that even
in formations characterized by abundant mineral phases known to strong
ly adsorb actinides, the actinides can be transported essentially cons
ervatively as NOM complexes. (C) 1998 Elsevier Science B.V.