Počet záznamů: 1
Geochemical, geotechnical and microbiological changes in mg/ca bentonite after thermal loading at 150 °C
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SYSNO ASEP 0545541 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Geochemical, geotechnical and microbiological changes in mg/ca bentonite after thermal loading at 150 °C Tvůrce(i) 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)Celkový počet autorů 9 Číslo článku 965 Zdroj.dok. Minerals. - : MDPI
Roč. 11, č. 9 (2021)Poč.str. 21 s. Jazyk dok. eng - angličtina Země vyd. CH - Švýcarsko Klíč. slova Cation exchange capacity ; Magnesium bentonite ; Microbial survivability ; Montmorillonite content ; Radioactive waste disposal ; Saturated hydraulic conductivity ; Water retention curves Vědní obor RIV CA - Anorganická chemie Obor OECD Inorganic and nuclear chemistry Způsob publikování Open access Institucionální podpora UACH-T - RVO:61388980 UT WOS 000701551800001 EID SCOPUS 85114265210 DOI 10.3390/min11090965 Anotace Bentonite 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. Pracoviště Ústav anorganické chemie Kontakt Jana Kroneislová, krone@iic.cas.cz, Tel.: 311 236 931 Rok sběru 2022 Elektronická adresa http://hdl.handle.net/11104/0322227
Počet záznamů: 1