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Uptake of actinides by calcium silicate hydrate (C-S-H) phases.

Authors :
Häußler, Verena
Amayri, Samer
Beck, Aaron
Platte, Tim
Stern, Tobias A.
Vitova, Tonya
Reich, Tobias
Source :
Applied Geochemistry. Nov2018, Vol. 98, p426-434. 9p.
Publication Year :
2018

Abstract

Abstract The sorption of actinides (Th, U – Am) was studied in dependence of the solid-to-liquid (S/L) ratio (0.5–20.0 g/L) and the calcium-to-silicon (C:S) ratio. The C:S ratio was varied between 1.80 and 0.70 to simulate the changing composition of the C-S-H phases during cement degradation from high to low C:S ratios. The decrease of the calcium content in the C-S-H phases by time is accompanied by a decrease in pH in the corresponding suspensions from 12.6 to 10.2. X-ray photoelectron spectroscopy (XPS) of the C-S-H phases showed an increasing depletion of Ca on the surface with increasing C:S ratio in comparison to the composition of the solid phase as a whole. The sorption experiments were performed with the redox stable species Am(III), Th(IV) and U(VI), as well as the redox sensitive Np(V) and Pu(III). The average distribution coefficients R d for all investigated actinides are around 105 L/kg. The oxidation state of Pu retained by the C-S-H phases was investigated with high-energy resolution X-ray absorption near-edge structure (HR-XANES) spectroscopy. Samples with C:S ratios of 0.75 and 1.65 showed that the initially added Pu(III) was oxidized to Pu(IV) in the course of the experiment. Graphical abstract Image 1 Highlights • First investigation of Pu uptake by C-S-H phases combining batch experiments with Pu M 5 -edge HR-XANES spectroscopy. • Similar R d values determined for Am(III), Pu(III), Th(IV), Np(V) and U(VI), independent of the C:S and S/L ratios. • XPS measurements indicate a depletion of Ca at the surface of the C-S-H phases. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
08832927
Volume :
98
Database :
Academic Search Index
Journal :
Applied Geochemistry
Publication Type :
Academic Journal
Accession number :
133068398
Full Text :
https://doi.org/10.1016/j.apgeochem.2018.08.021