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• W178465179 endingPage "412" @default.
• W178465179 startingPage "399" @default.
• W178465179 abstract "Increasing observations of subsurface actinide transport has reinforced the need for a basic geochemical and hydrologic understanding of how these contaminants are transported in groundwater. At the Nevada Test Site, NV, USA, low-levels of plutonium have been shown to migrate on the scale of kilometers. At all but one sampling location the Pu is associated with the colloidal fraction (<1 μm) consisting predominantly of clays and zeolites. The majority of the Pu (∼70%) is associated with the smallest nanoparticle (e.g., colloid) size fraction of 10–100 nm and in one case was identified as associated with a clay colloid. At one unique sampling site, Pu is predominantly associated with dissolved organic matter. Monitoring at over 20 contaminated groundwater sites at the NTS suggests that low-levels of Pu can be mobilized either via colloid-facilitated transport in fractured rock or as a result of aqueous Pu stabilization by anthropogenic levels of dissolved organic matter. Nevertheless, activities above the EPA’s Maximum Contaminant Level (MCL) for alpha-emitting radionuclides (15 pCi/L, 0.56 Bq/L) have been measured at only two locations at the NTS." @default.
• W178465179 created "2016-06-24" @default.
• W178465179 creator A5028978175 @default.
• W178465179 creator A5043297271 @default.
• W178465179 date "2011-01-01" @default.
• W178465179 modified "2023-10-14" @default.
• W178465179 title "Colloid-Facilitated Transport of Plutonium at the Nevada Test Site, NV, USA" @default.
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• W178465179 doi "https://doi.org/10.1007/978-3-642-11432-8_15" @default.
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