dc.contributor.author
Vettese, Gianni F.
dc.contributor.author
Li, Xiaodong
dc.contributor.author
Fairuz, Afrida
dc.contributor.author
Vierinen, Taavi
dc.contributor.author
Siren, Lilia
dc.contributor.author
Prieur, Damien
dc.contributor.author
Huittinen, Nina
dc.contributor.author
Law, Kathleen A.
dc.contributor.author
Bes, Rene
dc.contributor.author
Niskanen, Mika
dc.date.accessioned
2025-07-04T12:51:45Z
dc.date.available
2025-07-04T12:51:45Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/48145
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-47867
dc.description.abstract
Bentonite is a key barrier material in deep geological facilities for spent nuclear fuel, where it may be exposed to temperatures >100 °C because of radiogenic heating. Understanding how prolonged heating affects its physicochemical properties and radionuclide retention capacity is critical for ensuring long-term repository safety. This study investigated the impacts of dry heating (unconfined, evaporation allowed) at 150 °C for 36 months on the mineralogical and geochemical stability of a Wyoming bentonite, chosen for the Finnish geological disposal facility, and its subsequent sorption behavior with 90Sr. Although the bentonite mineralogy remained mostly stable, combined X-ray diffraction, cation exchange capacity, titrations, demonstrated partial Na to Ca exchange within montmorillonite's interlayer following heating, and specific surface area analyses revealed a > 50 % reduction in specific surface area (30 to 14 m2/g). Colloid stability tests revealed that bentonite colloids did not form under repository-relevant saline conditions (I = 0.2 M), and heat treatment did not significantly impact colloid formation in reduced ionic-strength systems. Sorption isotherms demonstrated that Sr sorption was strongly pH-dependent, increasing from ∼40 % at pH 8 to ∼90 % at pH 13, and heating slightly enhanced Sr retention at pH 8. Two-site protolysis non-electrostatic surface complexation and cation exchange modelling suggested that in unheated bentonite, Sr was bound via a combination of surface complexation (∼30 %) and cation exchange (∼70 %) at pH 8, while at pH 13, sorption shifted towards surface complexation. However, after heating, cation exchange dominated at both pH values. Extended X-ray absorption fine structure analysis confirmed outer-sphere Sr sorption at pH 8 and increasing inner-sphere complexation at pH 13. Together, these findings highlight that despite minor physicochemical alterations, bentonite retained its Sr sorption potential, supporting its continued suitability as a buffer material in the ONKALO® repository.
en
dc.format.extent
11 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
Bentonite buffer
en
dc.subject
Elevated temperature
en
dc.subject
Physicochemical alteration
en
dc.subject
Radio‑strontium sorption
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::540 Chemie::540 Chemie und zugeordnete Wissenschaften
dc.title
Effects of elevated temperature on Wyoming bentonite and its implications for sorption of radioactive strontium
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
107865
dcterms.bibliographicCitation.doi
10.1016/j.clay.2025.107865
dcterms.bibliographicCitation.journaltitle
Applied Clay Science
dcterms.bibliographicCitation.volume
274
dcterms.bibliographicCitation.url
https://doi.org/10.1016/j.clay.2025.107865
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
1872-9053
refubium.resourceType.provider
WoS-Alert