Environmental Mineralogy
Heavy Metal Adsorption onto Inorganic Colloids
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Colloids
are particles with dimensions between a nanometer and a micrometer.
Colloids can be mineral fragments, hydrolyzed metal agglomerations, humic or fulvic
acids, microbes, or clay or soil fragments: the definition is strictly
related to size, not composition. Because of their high surface area to volume ratios, colloids
are extremely surface active and can adsorb contaminants from solution.
Not only can this increase the concentration of the contaminant
in solution, but when adsorbed to the colloid the contaminant is present
in a potentially highly mobile form.
Indeed, colloids have enhanced subsurface transport of
radionuclides at numerous DOE facilities, as well as the Nevada Test
Site (NTS), the location of over 800 nuclear explosions and located
adjacent to the proposed radioactive waste repository at Yucca Mountain.
In addition, we are creating colloid suspensions from various Mn and Fe oxide minerals and adsorbing various metals (i.e., Ce, Cs, Sr, Se, and U) onto the colloids. Using HAADF-STEM we analyze the metal-bearing colloids and hope to discern fundamental knowledge about adsorption of radionuclides. For instance, does adsorption preferentially occur at surface defect sites, such as kinks, dislocation, or vacancies?. Publications Traexler, K. A.,
and Ewing, R.C. (January 2002) Colloid Formation and the Potential
Effects on Radionuclide Transport in a Geologic Repository for Spent
Nuclear Fuel. Department of
Energy. (DOE/SNF/REP-070). PDF
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