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The influence of uranyl hydrolysis and multiple site-binding reactions on adsorption of U(VI) to montmorillonite

James P. McKinley, John M. Zachara, Steven C. Smith and Gary D. Turner
The influence of uranyl hydrolysis and multiple site-binding reactions on adsorption of U(VI) to montmorillonite
Clays and Clay Minerals (October 1995) 43 (5): 586-598

Abstract

Adsorption of uranyl to SWy-1 montmorillonite was evaluated experimentally and results were modeled to identify likely surface complexation reactions responsible for removal of uranyl from solution. Uranyl was contacted with SWy-1 montmorillonite in a NaClO (sub 4) electrolyte solution at three ionic strengths (I = 0.001, 0.01, 0.1), at pH 4 to 8.5, in a N (sub 2(g)) ) atmosphere. At low ionic strength, adsorption decreased from 95% at pH 4 to 75% at pH 6.8. At higher ionic strength, adsorption increased with pH from initial values less than 75%; adsorption edges for all ionic strengths coalesced above a pH of 7. A site-binding model was applied that treated SWy-1 as an aggregate of fixed-charge sites and edge sites analogous to gibbsite and silica. The concentration of fixed-charge sites was estimated as the cation exchange capacity, and non-preference exchange was assumed in calculating the contribution of fixed-charge sites to total uranyl adsorption. The concentration of edge sites was estimated by image analysis of transmission electron photomicrographs. Adsorption constants for uranyl binding to gibbsite and silica were determined by fitting to experimental data, and these adsorption constants were then used to simulate SWy-1 adsorption results. The best simulations were obtained with an ionization model in which AlOH (sub 2) (super +) was the dominant aluminol surface species throughout the experimental range in pH. The pH-dependent aqueous speciation of uranyl was an important factor determining the magnitude of uranyl adsorption. At low ionic strength and low pH, adsorption by fixed-charge sites was predominant. The decrease in adsorption with increasing pH was caused by the formation of monovalent aqueous uranyl species, which were weakly bound to fixed-charge sites. At higher ionic strengths, competition with Na (super +) decreased the adsorption of UO (sub 2) (super 2+) to fixed-charge sites. At higher pH, the most significant adsorption reactions were the binding of UO (sub 2) (super 2+) to AIOH and of (UO (sub 2) ) (sub 3) (OH) (sub 5) (super +) to SiOH edge sites. Near-saturation of AlOH sites by UO (sub 2) (super 2+) allowed significant contributions of SiOH sites to uranyl adsorption.


ISSN: 0009-8604
Coden: CLCMAB
Serial Title: Clays and Clay Minerals
Serial Volume: 43
Serial Issue: 5
Title: The influence of uranyl hydrolysis and multiple site-binding reactions on adsorption of U(VI) to montmorillonite
Affiliation: Pacific Northwest Laboratory, Richland, WA, United States
Pages: 586-598
Published: 199510
Text Language: English
Publisher: Clay Minerals Society, Clarkson, NY, United States
References: 42
Accession Number: 1996-026572
Categories: Geochemistry of rocks, soils, and sedimentsSedimentary petrologyMineralogy of silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 4 tables
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, Copyright, Mineralogical Society of Great Britain and Ireland
Update Code: 199609
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