EGU23-1280
https://doi.org/10.5194/egusphere-egu23-1280
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

A multidisciplinary study to evaluate the sustainability of a volcanic hydrosystem: Chaîne des Puys’s watersheds use by Clermont Auvergne Métropole for drinking water supply

Cyril Aumar1,2, Pierre Nevers1, Hélène Celle1, Gilles Mailhot2, Frédéric Huneau3, Virginie Vergnaud4, Barbara Yvard4, and Marie-Laure Clauzet5
Cyril Aumar et al.
  • 1UMR 6249 CNRS Chrono-environnement, Université de Franche-Comté, F-25030 Besançon, France
  • 2CNRS, SIGMA Clermont, Institut de Chimie de Clermont-Ferrand, Université Clermont Auvergne, F-63000 Clermont-Ferrand, France
  • 3Université de Corse Pascal Paoli, Département d'Hydrogéologie, Campus Grimaldi, F-20250 Corte, France
  • 4Université de Rennes 1, OSUR, UMS 3343, Plateforme Condate Eau, F–35000 Rennes, France
  • 5Clermont Auvergne Métropole, Direction du Cycle de l'Eau, 58 Boulevard Berthelot, 63000 Clermont-Ferrand, France

Clermont Auvergne Métropole is an agglomeration of 300,000 inhabitants. Two types of aquifers are exploited for the drinking water supply of this population: the alluvial aquifer of Allier River (70%) and three volcanic water basins located in the Chaîne des Puys (30%). Recent studies have shown that the quantity of water in the Allier alluvial aquifer decreases drastically during drought periods and that this decrease will amplified in the future due to climate changes (2022 for example). Water managers of Clermont Auvergne Metropole are thus interested in identifying the potential of their volcanic resources to secure the water supply of the population. In this purpose, a multidisciplinary study, using existing data and providing new ones has been projected. This study includes: 1) the use of the geological model previously established by Aumar (2022) at the Chaîne des Puys scale, that allows to constrain the geometry of aquifers; 2) the acquisition of hydrochemical data that help to better define the functioning of the volcanic watersheds; 3) the measurement of hydrodynamic and meteorological data to better define the terms of the hydrological balance. Natural tracers such as stable water isotopes (18O and 2H) or major and trace elements give information on the origin of those groundwaters (local or remote) and in particular their infiltration zone (average altitudes), their flow paths or the impact of various external processes (environmental or anthropic). Groundwater dating methods (CFC, Tritium) brings a constraint on the residence time of water within the aquifer. Yet, groundwater ages are still unknown in all watersheds of the Chaîne des Puys, but it remains essential to understand groundwater flow and storage. The coupling between hydrodynamic monitoring, a large panel of hydrochemical tracers and groundwater residence time data associated with a well constrained geological model allows to provide relevant management tools to stakeholders both in terms of quantification and protection of their resources.  

How to cite: Aumar, C., Nevers, P., Celle, H., Mailhot, G., Huneau, F., Vergnaud, V., Yvard, B., and Clauzet, M.-L.: A multidisciplinary study to evaluate the sustainability of a volcanic hydrosystem: Chaîne des Puys’s watersheds use by Clermont Auvergne Métropole for drinking water supply, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-1280, https://doi.org/10.5194/egusphere-egu23-1280, 2023.