Uranium adsorption in sediments varies with respect to grain size

Uranium adsorption in sediments varies with respect to grain size
Scientists demonstrated a new concept that allows them to accurately calculate the uranium adsorption in a heterogeneous subsurface sample.

Using experimental and modeling resources at EMSL, scientists from the Pacific Northwest National Laboratory determined the equilibrium and kinetic properties of uranium(VI) adsorption to subsurface grains, which ranged in size from tiny clay particles to larger pieces of gravel. They found that the kinetics or the rate of adsorption onto the grains varies with respect to the grain size. Specifically, the larger-size grains adsorbed less uranium and did so at a slower rate than smaller grains. After determining the size-specific equilibrium and kinetic properties, the team created a series of mathematical formulas that allowed them to calculate uranium adsorption in a heterogeneous subsurface sample from the Hanford Site, a plutonium production complex in southeastern Washington State.

Uranium and other contaminants exist across large swaths of the Hanford Site subsurface. Calculating exactly how much uranium is present requires scientists to determine the adsorption behavior of the subsurface grains in the laboratory and then scale that knowledge to the field. This process has proven difficult for researchers in the past because of the heterogeneity of grain size distribution at the field.

The scientists on this study began by conducting a series of experiments to determine characteristics of different grain sizes. The experimental resources included surface area and microporosity instruments as well as stirred flow cells and other instrumentation. Following on the laboratory results, were done to quantify the kinetics and equilibrium thermodynamics. Then, the team developed appropriate formulas for adding the adsorptions to predict the uranium held in a larger sample.

The team tested their approach using a sample of contaminated Hanford Site sediment. Their approach agreed well with the measurements. The team is continuing to study this approach and will be moving on to determine the applicability to groundwater-infused sediments.


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More information: Shang, J, 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
Citation: Uranium adsorption in sediments varies with respect to grain size (2011, September 26) retrieved 21 August 2019 from https://phys.org/news/2011-09-uranium-adsorption-sediments-varies-respect.html
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Sep 26, 2011
Uranium adsorption in sediments varies with respect to grain size


Thanks for the story.

Since adsorption occurs at the surface, and the surface/volume ratio increases as grain size decreases, therefore adsorption depends on grain size.

Probably all surface processes depend on particle size:

Evaporation of water from droplets
Emission of neutrons from heavy nuclei
Condensation of Rn decay products on tobacco leaves
Condensation of water vapor on droplets
Capture of solar wind by lunar soil

With kind regards,
Oliver K. Manuel
Former NASA Principal
Investigator for Apollo

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