Hydrodynamic model for independent cold and thermo-mineral twin springs in a stratified continental karst aquifer, Camou, Arbailles Massif, Pyrénées, France

• Published in: International journal of speleology 2022-05, Vol.51 (2), p.81-91
• Main Authors: Audra, Philippe, Bigot, Jean-Yves, Laurent, Dimitri, Vanara, Nathalie, Cailhol, Didier, Cazenave, Gérard
• Format: Article
• Language: English
• Subjects: Aquifers; Carbonates; cave diving; Cold springs; Deep water; Density; Density gradients; Drainage; Earth Sciences; Environmental Sciences; Evaporites; Floodwater; Geography; hot hydrothermal plume; Humanities and Social Sciences; Hydrodynamics; Hydrology; hydrothermal component; hypogene karst; Karst; Massifs; Mineral springs; Mineralization; non-mixing flows; Pressure head; Sciences of the Universe; Stratification; Synclines; Thermocline; Triassic; various volumetric masses flows; Water bodies; Water springs
• ISSN: 0392-6672; 1827-806X
• DOI: 10.5038/1827-806X.51.2.2413

The Camou springs (Arbailles Massif, French Western Pyrenees) display an unusual close association of a typically cold karstic spring that drains the Urgonian western limb of the Arbailles, and a thermo-mineral spring (33.5°C; salinity 17.7 g/L). The latter gains its mineralization at the contact of Triassic evaporites mainly through a deep loop in the Apanicé syncline. The fast upflow of this deep water occurs at the cross of large active lines (the North-Pyrenean thrust located at depth, and the Saison transverse fault). Cave diving in the nearby Maddalen Cave allowed reaching the phreatic passage at the origin of the cold spring, which however also crosses the thermal body in the third sump (S3). Both water bodies are separated by a sharp thermocline. 6 pressure-temperature dataloggers were placed in both water bodies along the thermocline for 6 months. The dataloggers located downstream on either side of the thermocline show at the beginning of flood first a rise of the thermal body, then an invasion of the whole phreatic passage by the cold floodwater, controlled by head pressure changes in the karst aquifer. From observation of these mechanisms, we deduce a hydrodynamic model with a warm plume rising into the cold aquifer, without significant mixing. Such independence of water bodies is explained by the decrease of turbulent rate at the interface, due to the sharp density gradient. The relative absence of mixing does not actually require independent “watertight” routes, both water bodies can thus coexist even in the same conduit. This model locally implies the existence of unknown secondary passages close to the spring, which allow an independent draining of each water body toward separate outlets during low stage. Such type of stratified aquifer linked to density differences is common in coastal karst (Florida, French Calanques…), in the continental evaporite karst (Schlotten of the Harz in Germany, Kungur karst in Ural…), but remains poorly identified in continental carbonate karst areas, mainly because of the difficulty of access. Together with the Mescla spring in French Alpes-Maritimes, the Camou twin springs discharging in the same porch are an outstanding example, allowing a direct study of the stratification and the dynamic of highly contrasted water bodies.