Contributors: Institut Terre Environnement Strasbourg (ITES); École Nationale du Génie de l'Eau et de l'Environnement de Strasbourg (ENGEES)-Université de Strasbourg (UNISTRA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS); Observatoire des sciences de l'univers Ecce Terra Paris (OSU ECCE TERRA); École normale supérieure - Paris (ENS-PSL); Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS); Milieux Environnementaux, Transferts et Interactions dans les hydrosystèmes et les Sols (METIS); École Pratique des Hautes Études (EPHE); Géosciences Montpellier; Université des Antilles et de la Guyane (UAG)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS); IMPT (CNRS); Prime 80 de la MITI (CNRS); OZCAR-TERENO; ANR-24-CE56-3383,CASH,Inversion hydrogéophysique à l'échelle du bassin versant(2024); ANR-11-EQPX-0011,CRITEX,Parc national d'équipements innovants pour l'étude spatiale et temporelle de la Zone Critique des Bassins Versants(2011); ANR-15-CE01-0010,HYDROCRIZSTO,Combinaison d'études géophysiques, hydrologiques et géochimiques pour mieux caractériser, comprendre et modéliser le fonctionnement passé, actuel et futur de bassins versants.(2015)
نبذة مختصرة : International audience ; The Strengbach headwater catchment has been monitored since 1986 by the OHGE (Observatoire Hydrogéochimique de l’Environnement) critical zone observatory. Located in the Vosges mountains (northeastern France) with altitudes ranging from 880 m and 1150 m, the 0.8 km² catchment lies on a granitic bedrock. Meteorological and hydrological data are continuously monitored and six boreholes highlight the underground structure down to depths of 50 to 120 m, providing information on the distribution of geological facies.Particularities of this site, such as its relatively thin porous media, compared to sedimentary contexts and its strong topography have encouraged the application of challenging geophysical experiments. Thus, magnetic resonance soundings, which can provide estimates of water contents, were acquired to explore the potential of the method to detect the water content despite the expected low values. Similarly, gravity measurements were acquired to assess whether the method can detect groundwater variations over time despite the strong topography and the poorly known groundwater fluctuations. In addition, seismic refraction tomographies were acquired to provide information on the geometry of hydrofacies. While those experiments were set up separately, we’ll show how they provide complementary insights and could be integrated within a single workflow to solve the hydrological inverse problem at the catchment scale.
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