Modeling uranium(VI) adsorption onto montmorillonite under varying carbonate concentrations: A surface complexation model accounting for the spillover effect on surface potential
Abstract
The prediction of U(VI) adsorption onto montmorillonite clay is confounded by the complexities of: (1) the montmorillonite structure in terms of adsorption sites on basal and edge surfaces, and the complex interactions between the electrical double layers at these surfaces, and (2) U(VI) solution speciation, which can include cationic, anionic and neutral species. Previous U(VI)-montmorillonite adsorption and modeling studies have typically expanded classical surface complexation modeling approaches, initially developed for simple oxides, to include both cation exchange and surface complexation reactions. However, previous models have not taken into account the unique characteristics of electrostatic surface potentials that occur at montmorillonite edge sites, where the electrostatic surface potential of basal plane cation exchange sites influences the surface potential of neighboring edge sites (‘spillover’ effect).
- Authors:
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Nuclear Energy (NE)
- OSTI Identifier:
- 1437748
- Alternate Identifier(s):
- OSTI ID: 1419466
- Grant/Contract Number:
- AC02-05CH11231
- Resource Type:
- Journal Article: Published Article
- Journal Name:
- Geochimica et Cosmochimica Acta
- Additional Journal Information:
- Journal Name: Geochimica et Cosmochimica Acta Journal Volume: 220 Journal Issue: C; Journal ID: ISSN 0016-7037
- Publisher:
- Elsevier
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; 54 ENVIRONMENTAL SCIENCES; Uranium; Adsorption; Clay; Montmorilonite; Spillover; Surface complexation modeling
Citation Formats
Tournassat, C., Tinnacher, R. M., Grangeon, S., and Davis, J. A. Modeling uranium(VI) adsorption onto montmorillonite under varying carbonate concentrations: A surface complexation model accounting for the spillover effect on surface potential. United States: N. p., 2018.
Web. doi:10.1016/j.gca.2017.09.049.
Tournassat, C., Tinnacher, R. M., Grangeon, S., & Davis, J. A. Modeling uranium(VI) adsorption onto montmorillonite under varying carbonate concentrations: A surface complexation model accounting for the spillover effect on surface potential. United States. https://doi.org/10.1016/j.gca.2017.09.049
Tournassat, C., Tinnacher, R. M., Grangeon, S., and Davis, J. A. 2018.
"Modeling uranium(VI) adsorption onto montmorillonite under varying carbonate concentrations: A surface complexation model accounting for the spillover effect on surface potential". United States. https://doi.org/10.1016/j.gca.2017.09.049.
@article{osti_1437748,
title = {Modeling uranium(VI) adsorption onto montmorillonite under varying carbonate concentrations: A surface complexation model accounting for the spillover effect on surface potential},
author = {Tournassat, C. and Tinnacher, R. M. and Grangeon, S. and Davis, J. A.},
abstractNote = {The prediction of U(VI) adsorption onto montmorillonite clay is confounded by the complexities of: (1) the montmorillonite structure in terms of adsorption sites on basal and edge surfaces, and the complex interactions between the electrical double layers at these surfaces, and (2) U(VI) solution speciation, which can include cationic, anionic and neutral species. Previous U(VI)-montmorillonite adsorption and modeling studies have typically expanded classical surface complexation modeling approaches, initially developed for simple oxides, to include both cation exchange and surface complexation reactions. However, previous models have not taken into account the unique characteristics of electrostatic surface potentials that occur at montmorillonite edge sites, where the electrostatic surface potential of basal plane cation exchange sites influences the surface potential of neighboring edge sites (‘spillover’ effect).},
doi = {10.1016/j.gca.2017.09.049},
url = {https://www.osti.gov/biblio/1437748},
journal = {Geochimica et Cosmochimica Acta},
issn = {0016-7037},
number = C,
volume = 220,
place = {United States},
year = {Mon Jan 01 00:00:00 EST 2018},
month = {Mon Jan 01 00:00:00 EST 2018}
}
Web of Science
Works referencing / citing this record:
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