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Geochemical, geotechnical and microbiological changes in mg/ca bentonite after thermal loading at 150 °C

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    SYSNO ASEP0545541
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleGeochemical, geotechnical and microbiological changes in mg/ca bentonite after thermal loading at 150 °C
    Author(s) Kašpar, V. (CZ)
    Šachlová, Š. (CZ)
    Hofmanová, E. (CZ)
    Komárková, Bára (UACH-T) RID, SAI, ORCID
    Havlová, V. (CZ)
    Aparicio, C. (CZ)
    Černá, K. (CZ)
    Bartak, D. (CZ)
    Hlaváčková, V. (CZ)
    Number of authors9
    Article number965
    Source TitleMinerals. - : MDPI
    Roč. 11, č. 9 (2021)
    Number of pages21 s.
    Languageeng - English
    CountryCH - Switzerland
    KeywordsCation exchange capacity ; Magnesium bentonite ; Microbial survivability ; Montmorillonite content ; Radioactive waste disposal ; Saturated hydraulic conductivity ; Water retention curves
    Subject RIVCA - Inorganic Chemistry
    OECD categoryInorganic and nuclear chemistry
    Method of publishingOpen access
    Institutional supportUACH-T - RVO:61388980
    UT WOS000701551800001
    EID SCOPUS85114265210
    DOI10.3390/min11090965
    AnnotationBentonite buffers at temperatures beyond 100 °C could reduce the amount of high-level radioactive waste in a deep geological repository. However, it is necessary to demonstrate that the buffer surrounding the canisters withstands such elevated temperatures, while maintaining its safety functions (regarding long-term performance). For this reason, an experiment with thermal loading of bentonite powder at 150 °C was arranged. The paper presents changes that the Czech Mg/Ca bentonite underwent during heating for one year. These changes were examined by X-ray diffraction (XRD), thermal analysis with evolved gas analysis (TA-EGA), aqueous leachates, Cs sorption, cation exchange capacity (CEC), specific surface area (SSA), free swelling, saturated hydraulic conductivity, water retention curves (WRC), quantitative polymerase chain reaction (qPCR), and next-generation sequencing (NGS). It was concluded that montmorillonite was partially altered, in terms of the magnitude of the surface charge density of montmorillonite particles, based on the measurement interpretations of CEC, SSA, and Cs sorption. Montmorillonite alteration towards low-or non-swelling clay structures corresponded well to significantly lower swelling ability and water uptake ability, and higher saturated hydraulic conductivity of thermally loaded samples. Microbial survivability decreased with the thermal loading time, but it was not completely diminished, even in samples heated for one year.
    WorkplaceInstitute of Inorganic Chemistry
    ContactJana Kroneislová, krone@iic.cas.cz, Tel.: 311 236 931
    Year of Publishing2022
    Electronic addresshttp://hdl.handle.net/11104/0322227
Number of the records: 1  

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