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Ternary uranyl-citrate-surface complex formation on geothite gibbsite, and phylosilicate minerals

Conference ·
OSTI ID:370507
; ;  [1]
  1. Stanford Univ., CA (United States)
Liquid radioactive wastes that contain transuranic elements are often associated with complexing organic co-contaminants. Prediction of radionuclide transpose in contaminated groundwater will require accounting for the effect of both organic co-solutes and naturally occurring compounds. A study has been conducted on the adsorption of uranyl ion (UO{sub 2}{sup 2+}) on goethite, gibbsite, and phylosilicate minerals in the presence of varying concentrations of citric acid. Adsorption of either solute separately as functions of pH yield sorption curves that are generally typical for cations and anions with differences in features reflecting differences in properties of the surface functional groups. At equimolar concentrations of uranyl and citrate little effect on the sorption of either solute is observed. However, at higher citrate concentrations uranyl sorption dramatically increases with nearly complete uranyl sorption even at relatively low pH values. A stable bridging structure involving uranyl and citrate is implied. These results have significant relevance to radionuclide transport modeling where soluble chelators may increase rather than decrease sorption of uranyl.
OSTI ID:
370507
Report Number(s):
CONF-960376--
Country of Publication:
United States
Language:
English

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