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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGODINAUD, Jeremy
hal.structure.identifierGéosciences Rennes [GR]
dc.contributor.authorKLEPIKOVA, Maria
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLARROQUE, Francois
hal.structure.identifierGéosciences Rennes [GR]
dc.contributor.authorGUIHÉNEUF, Nicolas
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDUPUY, Alain
hal.structure.identifierGéosciences Rennes [GR]
dc.contributor.authorBOUR, Olivier
dc.date.accessioned2024-03-07T09:33:29Z
dc.date.available2024-03-07T09:33:29Z
dc.date.issued2023
dc.identifier.issn0022-1694en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/188620
dc.description.abstractEnFiber-Optic Active Distributed Temperature Sensing (FO-ADTS) experiments were performed on an Aquifer Thermal Energy Storage system (ATES) site located on the university campus of Bordeaux, France. The experiments consisted in heating the steel core of the FO cable while monitoring the rate of temperature increase during the heating periods. The changes in temperature, that were monitored through time at every depth under various hydraulic conditions and in different boreholes, were used to evaluate both aquifer properties and wells conditions. A first ADTS experiment was conducted under cross borehole configuration using a pumping well and a monitoring well separated by a distance of 8.5 meters. Then, to check the reciprocity of the results, a second experiment was conducted by switching the monitoring and the pumping well. The results obtained through the use of analytical solutions for reproducing and interpreting the data lead to the following conclusions: (i) ADTS can be used to estimate both thermal conductivity and Darcy velocity distribution along boreholes, crucial properties for ATES performance. (ii) The proposed method is a promising tool to detect clogging locations in the boreholes when it occurs. This can be of great practical interest to maintain systems performance, since, once FO cables deployed, experiments could be easily repeated without opening boreholes and stop the system operation.
dc.description.sponsorshipParc national d'équipements innovants pour l'étude spatiale et temporelle de la Zone Critique des Bassins Versants - ANR-11-EQPX-0011en_US
dc.language.isoENen_US
dc.subject.enDistributed Temperature Sensing
dc.subject.enGroundwater Flux
dc.subject.enThermal Conductivity
dc.subject.enClogging
dc.subject.enATES
dc.title.enClogging detection and productive layers identification along boreholes using Active Distributed Temperature Sensing
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.jhydrol.2023.129113en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Hydrologieen_US
dc.description.sponsorshipEuropeTransport of Heat in hEteRogeneous Media - Marie-Sklodowska Curieen_US
bordeaux.journalJournal of Hydrologyen_US
bordeaux.page129113en_US
bordeaux.volume617en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issuePart Cen_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPROMESSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierinsu-03955737
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
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