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Published on: June 21, 2015
Phosphate controls uranium release from acidic waste-weathered Hanford sediments
Angélica Vázquez-Ortega1, Nicolas Perdrial2, Estela Reinoso-Maset3
1Department of Environmental Science, University of Arizona, 1177 East Fourth Street, Tucson, ARI 85721, USA; School of Earth, Environment and Society, Bowling Green State University, 190 Overman Hall, Bowling Green, OH 43403, USA.
Phosphate addition stabilizes uranium (U) in contaminated sediments by forming recalcitrant uranyl minerals. This prevents U release when exposed to infiltrating water, crucial for managing radioactive waste sites.
Area of Science:
- Environmental Science
- Geochemistry
- Radiochemistry
Background:
- Contaminant fate in soils and sediments is governed by mineral dissolution and precipitation.
- Aggressive solutions can transform native minerals, releasing incorporated contaminants via water percolation.
Purpose of the Study:
- To evaluate uranium (U) release from Hanford sediments after reaction with U-containing liquid waste.
- To investigate the influence of phosphate on U release and mineral transformation.
Main Methods:
- Flow-through column experiments using Hanford sediments reacted with U-containing solutions (with/without phosphate) at pH 2 and 3.
- Simulated background porewater (BPW; pH ~7) leaching for 22 days.
- Uranium LIII-edge EXAFS spectroscopy and thermodynamic calculations.
Main Results:
- Up to 5% U release from phosphate-free sediments due to becquerelite and boltwoodite dissolution.
- Negligible U release from phosphate-reacted sediments, with meta-ankoleite as the main U-mineral phase.
- Becquerelite and meta-ankoleite transformed into schoepite and phosphuranylite-type phases, respectively.
Conclusions:
- Phosphate addition stabilizes U in sediments by forming recalcitrant uranyl minerals.
- This stabilization significantly reduces U release upon exposure to infiltrating porewater.
- Phosphate plays a key role in controlling U mobility and release at contaminated sites.
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