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Characterization of Eu(III) co-precipitated with and adsorbed on hectorite: from macroscopic crystallites to nanoparticles

Published online by Cambridge University Press:  05 July 2018

N. Finck ,
M. Bouby ,
K. Dardenne  and
H. Geckeis
N. Finck*
Affiliation:
Institute for Nuclear Waste Disposal (INE), Karlsruhe Institute of Technology (KIT), PO Box 3640, D-76021 Karlsruhe, Germany
M. Bouby
Affiliation:
Institute for Nuclear Waste Disposal (INE), Karlsruhe Institute of Technology (KIT), PO Box 3640, D-76021 Karlsruhe, Germany
K. Dardenne
Affiliation:
Institute for Nuclear Waste Disposal (INE), Karlsruhe Institute of Technology (KIT), PO Box 3640, D-76021 Karlsruhe, Germany
H. Geckeis
Affiliation:
Institute for Nuclear Waste Disposal (INE), Karlsruhe Institute of Technology (KIT), PO Box 3640, D-76021 Karlsruhe, Germany
*
*E-mail: [email protected]
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Abstract

Hectorite was synthesized from a Eu(III)-bearing brucite precursor in a multistep procedure. In a separate experiment, Eu(III) ions were adsorbed onto hectorite in suspension. Colloids were extracted from both samples. The size distributions in the colloidal fractions were characterizedby application of the asymmetrical flow field-flow fractionation (AsFlFFF) method and the corresponding elemental compositions were obtained by ICP-MS. Extended X-ray absorption fine structure (EXAFS) spectroscopy was used to characterize the local chemical environment surrounding Eu in thebulk samples and in the colloidal fractions.

The EXAFS results show that Eu is associated with hectorite upon co-precipitation or adsorption. Results from AsFlFFF suggest that Eu is structurally associated with the colloidal fraction extracted from bulk Eu-bearing co-precipitated hectorite.The AsFlFFF data are different for the colloidal fraction containing Eu(III) adsorbed on hectorite; in this sample they are consistent with a surface retention mechanism. These small but significant differences enable surface sorbed Eu to be distinguished from co-precipitated Eu. Eu is verylikely located in a clay-like environment in the co-precipitation experiment, and it forms inner-sphere surface complexes in the adsorption experiment. The results obtained using the different experimental techniques agree, and show the benefits of using multiple methods of analysis.

Trivalent europium was used as non-radioactive chemical homologue for trivalent actinides. Similar retention mechanisms are expected for the trivalent actinides if they are co-precipitating with or adsorbing onto sheet silicates. The present study provides information which can be usefullyadded to the safety assessments required for deeply buried nuclear waste disposal sites.

Keywords

europiumhectoriteASFLFFFexafsnuclear wastegeological disposal
Type
Research Article
Information
Mineralogical Magazine , Volume 76 , Issue 7 , December 2012 , pp. 2723 - 2740
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2016

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