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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorROSSI, Lena
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLOISY, Corinne
IDREF: 155424866
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCEREPI, Adrian
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLE ROUX, Olivier
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorESTUBLIER, Audrey
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorNOIREZ, Sonia
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorMARTIN, Frédéric
hal.structure.identifierGLINCS SAS
dc.contributor.authorHAUTEFEUILLE, Benoit
hal.structure.identifierGLINCS SAS
dc.contributor.authorBRICHART, Thomas
hal.structure.identifierIFP Energies nouvelles [IFPEN]
dc.contributor.authorGARCIA, Bruno
dc.date.accessioned2025-04-02T07:25:02Z
dc.date.available2025-04-02T07:25:02Z
dc.date.issued2024-02
dc.identifier.issn1750-5836en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/205888
dc.description.abstractEnTo investigate the role of hydrogeological conditions on the release of major and trace elements during CO2 leakage occurring in shallow freshwater aquifers in a CO2 Capture and Storage context, this paper compares the results of two in-situ CO2 leakage experiments. These experiments were carried out in a shallow freshwater carbonated aquifer located in Saint-Emilion, France, during both low and high-water levels periods. In both experiments, 200 L of carbonated water were injected into a well and groundwater monitoring was carried out downstream.Due to the physical heterogeneity of the aquifer at a small scale, the CO2-rich water plume did not follow the same flow path between the two hydrogeological periods, thus highlighting preferential pathways. It was observed that geochemical changes were not of the same intensity. The concentrations of Ca2+, HCO3−, Mg2+, Fe, Mn, As, Co, Cu, Ba, Sr and V increased during the low-water level experiment while the measured concentrations only reflected the dilution of the gasified water injected during the high-water level period.
dc.language.isoENen_US
dc.subject.enField experiment
dc.subject.enCarbonate aquifer
dc.subject.enCO2-rock-water interactions
dc.subject.enHydrogeological conditions
dc.subject.enEnvironmental impact
dc.subject.enGeochemical modelling
dc.title.enImpact of a CO2 leak on the release of major and trace elements according to groundwater flow conditions in a shallow freshwater carbonate aquifer: In-situ experiments and modelling
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.ijggc.2023.104042en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terreen_US
bordeaux.journalInternational Journal of Greenhouse Gas Controlen_US
bordeaux.page104042en_US
bordeaux.volume132en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04920810
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
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