dc.contributor.author
Schmeide, Katja
dc.contributor.author
Huittinen, Nina M.
dc.contributor.author
Shams Aldin Azzam, Salim
dc.contributor.author
Bok, Frank
dc.contributor.author
Brendler, Erica
dc.contributor.author
Lothenbach, Barbara
dc.contributor.author
Kretzschmar, Jerome
dc.date.accessioned
2025-09-08T12:46:51Z
dc.date.available
2025-09-08T12:46:51Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/49165
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-48888
dc.description.abstract
Calcium aluminosilicate hydrates (C-A-S-H) are the main hydration products of cement formulations with Al-rich additives such as blast furnace slags, fly ashes or calcined clays. We studied systematically the effect of Al substitution on both the structure of C-A-S-H phases and their U(VI) retention properties in comparison to C-S-H phases. To represent the different stages of cement degradation, three series of samples were synthesized, which included samples with Ca/Si molar ratios of 0.8, 1.2 and 1.6 and different Al/Si molar ratios of 0, 0.06 and 0.18 for each series. Furthermore, the impact of synthesis temperature (room temperature, 100 °C, 200 °C) on the C-(A-)S-H structure was studied. The U(VI) retention, studied either by sorption experiments or by direct synthesis of U(VI)-containing C-(A-)S-H phases, was found to be strong with log Rd between 4.9 and 5.6. Structural characteristics of the cementitious phases were obtained from powder X-ray diffraction (XRD) as well as 29Si and 27Al solid-state magic angle spinning nuclear magnetic resonance (SS MAS NMR) spectroscopy. AlO4 tetrahedra were identified to occupy bridging positions of the silicate chains, thereby increasing the mean chain length and providing additional sorption sites for U(VI) at room temperature. Elevated temperatures during solid phase formation, however, lead to a stronger cross-linking of the silicate chains with the appearance of neoformed crystalline phases. Luminescence spectroscopy was applied to characterize the U(VI) binding. Various U(VI) species (interlayer or surface sorbed) are formed in different proportions, depending on the composition and structure of the C-(A-)S-H phases, which are partly affected by elevated temperatures. To simulate salinity changes of the pore water, the effect of enhanced ionic strengths and the presence of carbonate on the stability of the U(VI) retention by the C-(A-)S-H phases was studied by sorption and leaching experiments over extended timescales of up to 6 months. For C-(A-)S-H phases previously exposed to temperatures of up to 100 °C, the effect of medium ionic strengths (up to 2.6 M) on U(VI) retention was insignificant.
en
dc.format.extent
15 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
Radionuclide
en
dc.subject
Hydrothermal synthesis
en
dc.subject
Luminescence
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::540 Chemie::540 Chemie und zugeordnete Wissenschaften
dc.title
Uranium(VI) retention by calcium (alumino)silicate hydrates – Impact of temperature and ionic strength
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
106400
dcterms.bibliographicCitation.doi
10.1016/j.apgeochem.2025.106400
dcterms.bibliographicCitation.journaltitle
Applied Geochemistry
dcterms.bibliographicCitation.volume
186
dcterms.bibliographicCitation.url
https://doi.org/10.1016/j.apgeochem.2025.106400
refubium.affiliation
Biologie, Chemie, Pharmazie
refubium.affiliation.other
Institut für Chemie und Biochemie

refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
1872-9134
refubium.resourceType.provider
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