The preferences of uranium: Radionuclide's adsorption in Hanford Site sediments varies based on grain size

Oct 25, 2011
The Preferences of Uranium
More than 200,000 kg of uranium have been released to the vadose zone at the Hanford Site. Plumes of uranium exist in the groundwater and vadose zone.

(PhysOrg.com) -- Uranium prefers petite particles. The radionuclide attaches quickly and abundantly to smaller subsurface grains, according to scientists at Pacific Northwest National Laboratory. The team found that gravel and other large bits adsorbed less uranium(IV) than smaller grains. The larger particles also adsorbed uranium more slowly than the smaller ones. Using this information, the team wrote a series of mathematical formulas to predict uranium adsorption and desorption affinity and kinetics in sediments containing different grain sizes. The predictions were successfully tested using sediment from the Hanford Site.

Uranium movement at the Hanford Site is an ongoing concern. Uranium and other radioactive holdovers from weapons production reside under the Site, in southeastern Washington State. These are spreading out from their sources and migrating toward the , a major waterway. To keep the uranium from the river, scientists need to know how uranium moves, or doesn't, through the complex subsurface. This study demonstrates a way for getting such information for wide areas. With these and other results, PNNL scientists are shaping how uranium's behavior is considered by scientists, cleanup experts, and regulators.

Calculating exactly how much uranium is present and how fast uranium migrates requires scientists to scale measurements from the lab to the field. Essentially, they must take samples measured across millimeters to centimeters and extrapolate them to systems that extend for meters or kilometers.

"Upscaling is always a challenge," said Dr. Chongxuan Liu, a PNNL who worked on the study.

The scientists on this study began by conducting experiments to determine adsorption characteristics of four grain sizes. The grains were coarse sand (1-2 mm), medium sand (0.2-1 mm), fine sand (0.053-0.2 mm), and clay/silt fraction (<0.053 mm). The scientists used surface area and microporosity instruments, stirred flow cells, and other resources at EMSL. Based on the experimental results, they performed computer simulations to quantify the kinetics and equilibrium thermodynamics in individual size fractions.

Scientists demonstrated a new concept that allows them to accurately calculate the uranium adsorption in a heterogeneous subsurface sample.

Then, the team worked out to sum up the uranium adsorptions in the sediments consisting of different grain sizes. The team tested their approach using contaminated Hanford Site sediment. Their calculations agreed well with the laboratory measurements.

The team is continuing to examine this approach, drawing upon PNNL's nearly 50 years of geochemistry and biogeochemistry experience. Next, the team will determine if their approach is robust under variable geochemical and hydrological conditions at Hanford Site.

Explore further: New water balance calculation for the Dead Sea

More information: J Shang, et al. 2011. "Effect of Grain Size on Uranium(VI) Surface Complexation Kinetics and Adsorption Additivity." Environmental Science & Technology 45(14):6025-6031. DOI:10.1021/es200920k

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