Hidrogeología del Karst de Pico Frentes (Cordillera Ibérica, España)

The karst system of Pico Frentes has developed within an Upper Cretaceous calcareous series whose well-defined folded geometry determines that its aquifer reserves are held mainly in three hydraulically-connected synclines, with a groundwater capacity of between 5 and 7 hm 3 . The recharge to this unconfined peneplain aquifer is autogenous and diffuse. On a large scale, groundwater flow is directed by the base of the synclines, while on a small scale, it flows along groundwater conduits towards the Fuentetoba Spring (210 l/s) and source of the River Mazos (50 l/s), following a highly variable flow regime of low inertia, with other smaller discharges emanating during periods of high water. Analysis of hydrographs of these springs indicates a very variable rate system and little power regulating natural, characteristic of a typical karstic aquifer, with great capacity for renewal and low residence time. Using hydrogram simulations of these upwellings using a mathematical rainfall-runoff model, a detailed quantification of the average water balance was made for a twenty-year time series. This water balance consists of 16,86 hm 3 rainfall (100%); natural recharge, 8,35 hm 3 (49,53%); EVT 8,50 hm 3 (50,41%); pumped groundwater abstractions, 0,01hm 3 (0,06%); surface runoff, 0 hm 3 , groundwater transfers to other aquifer, 0 hm 3 .