Effect of Fulvic Acid Surface Coatings on Plutonium Sorption and Desorption Kinetics on Goethite
Author(s) -
Ruth M. Tinnacher,
James D. Begg,
Harris E. Mason,
James F. Ranville,
Brian A. Powell,
Jennifer C. Wong,
Annie B. Kersting,
Mavrik Zavarin
Publication year - 2015
Publication title -
environmental science and technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.851
H-Index - 397
eISSN - 1520-5851
pISSN - 0013-936X
DOI - 10.1021/es505120s
Subject(s) - goethite , sorption , chemistry , desorption , plutonium , kinetics , organic matter , humic acid , environmental chemistry , natural organic matter , adsorption , inorganic chemistry , nuclear chemistry , organic chemistry , fertilizer , physics , quantum mechanics
The rates and extent of plutonium (Pu) sorption and desorption onto mineral surfaces are important parameters for predicting Pu mobility in subsurface environments. The presence of natural organic matter, such as fulvic acid (FA), may influence these parameters. We investigated the effects of FA on Pu(IV) sorption/desorption onto goethite in two scenarios: when FA was (1) initially present in solution or (2) found as organic coatings on the mineral surface. A low pH was used to maximize FA coatings on goethite. Experiments were combined with kinetic modeling and speciation calculations to interpret variations in Pu sorption rates in the presence of FA. Our results indicate that FA can change the rates and extent of Pu sorption onto goethite at pH 4. Differences in the kinetics of Pu sorption were observed as a function of the concentration and initial form of FA. The fraction of desorbed Pu decreased in the presence of FA, indicating that organic matter can stabilize sorbed Pu on goethite. These results suggest that ternary Pu-FA-mineral complexes could enhance colloid-facilitated Pu transport. However, more representative natural conditions need to be investigated to quantify the relevance of these findings.
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