δ 18 O/δ 2 H and 87 Sr/ 86 Sr in supporting understanding a complex karstic system linked to surface water -The Loiret system, France

The project CENARI-O aimed at improving knowledge on groundwater-surface water exchanges in a complex karstic area modified by hydraulic infrastructures combining various tools. The results obtained using δ18O/ δ2H and 87Sr/86Sr were compared to in situ conductivity and temperature measurements in order to complete the information. The Loiret River is mainly fed by groundwater along its flow path. This very particular flow system is more complex and various tools were needed to improve surface-groundwater knowledge.

Mots clés

stable isotopes river interaction alluvial aquifer

Domaines

Milieux et Changements globaux Sciences de l'ingénieur [physics]

Fichier principal

poster_cenario_Gourcy_312.pdf (532.61 Ko)

GOURCY_2023_IHS_Synopsis.pdf (519.06 Ko)

Origine	Fichiers produits par l'(les) auteur(s)

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https://brgm.hal.science/hal-04131995

Soumis le : samedi 17 juin 2023-20:43:05

Dernière modification le : vendredi 6 septembre 2024-16:20:03

Archivage à long terme le : lundi 18 septembre 2023-18:23:28

Dates et versions

hal-04131995 , version 1 (17-06-2023)

Identifiants

HAL Id : hal-04131995 , version 1

Citer

Laurence Gourcy, Emmanuelle Petelet-Giraud, Chrystelle Auterives, Stéphane Binet, Célestine Delbart, et al.. δ 18 O/δ 2 H and 87 Sr/ 86 Sr in supporting understanding a complex karstic system linked to surface water -The Loiret system, France. International Symposium on Isotope Hydrology: Sustainable Water Resources in a Changing World, Jul 2023, Vienne, Austria. . ⟨hal-04131995⟩

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