Prediction of Long-Term Geochemical Change in Bentonite Based on the Interpretative THMC Model of the FEBEX In Situ Test

dc.contributor.authorZheng, Liange
dc.contributor.authorFernández, Ana María
dc.date.accessioned2025-01-29T22:37:25Z
dc.date.available2025-01-29T22:37:25Z
dc.date.issued2023-12-05
dc.description.abstractSince nuclear energy is crucial in the decarbonization of the energy supply, one hurdle to remove is the handling of high-level radioactive waste (HLW). Disposal of HLW in a deep geological repository has long been deemed a viable permanent option. In the design of a deep geological repository, compacted bentonite is the most commonly proposed buffer material. Predicting the longterm chemical evolution in bentonite, which is important for the safety assessment of a repository, has been challenging because of the complex coupled processes. Models for large-scale tests and predictions based on such models have been some of the best practices for such purposes. An 18-yearlong in situ test with two dismantling events provided a unique set of chemical data that allowed for studying chemical changes in bentonite. In this paper, we first developed coupled thermal, hydrological, mechanical, and chemical (THMC) models to interpret the geochemical data collected in the in situ test and then extended the THMC model to 200 years to make long-term prediction of the geochemical evolution of bentonite. The interpretive coupled THMC model shows that the geochemical profiles were strongly affected by THM processes such as evaporation/condensation, porosity change caused by swelling, permeability change, and the shape of concentration profiles for major cations were largely controlled by transport processes, but concentration levels were regulated by chemical reactions, and the profiles of some species such as pH, bicarbonate, and sulfate were dominated by these reactions. The long-term THMC model showed that heating prolongs the time that bentonite becomes fully saturated in the area close to the heater/canister; however, once the bentonite becomes fully saturated, high concentrations of ions in bentonite near the heater, which was observed in the field test, will disappear; illitization continues for 50 years but will not proceed further.es_ES
dc.description.sponsorshipThis research was funded by the Spent Fuel andWaste Science and Technology, Office of Nuclear Energy, of the U.S. Department of Energy under Contract Number DE-AC02-05CH11231 with Lawrence Berkeley National Laboratory.es_ES
dc.identifier.citationZheng, L.; Fernández, A.M. Prediction of Long-Term Geochemical Change in Bentonite Based on the Interpretative THMC Model of the FEBEX In Situ Test. Minerals 2023, 13, 1522. https://doi.org/10.3390/ min13121522es_ES
dc.identifier.issn2075-163X
dc.identifier.urihttps://hdl.handle.net/20.500.14855/4472
dc.language.isoenges_ES
dc.relation.ispartofseriesMinerals;13
dc.rights.accessRightsopen accesses_ES
dc.subjectHigh-level radioactive wastees_ES
dc.subjectRepositoryes_ES
dc.subjectbentonitees_ES
dc.subjectModeles_ES
dc.subjectTHMCes_ES
dc.subjectField Testes_ES
dc.subjectgeochemicales_ES
dc.subjectlong-termes_ES
dc.subjectpredictiones_ES
dc.titlePrediction of Long-Term Geochemical Change in Bentonite Based on the Interpretative THMC Model of the FEBEX In Situ Testes_ES
dc.typejournal articlees_ES

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