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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 7 | Copyright

Special issue: Cold region hydrology: improved processes, parameterization...

Hydrol. Earth Syst. Sci., 13, 1261-1271, 2009
https://doi.org/10.5194/hess-13-1261-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  21 Jul 2009

21 Jul 2009

The hydrological response of baseflow in fractured mountain areas

A. Millares1, M. J. Polo2, and M. A. Losada1 A. Millares et al.
  • 1Environmental Fluid Dynamic Group, Andalusian Centre for Environmental Studies (CEAMA), Avda. del Mediterráneo s/n. 18006, Granada, Spain
  • 2Hydrology and Hydraulics in Agriculture Research Group, University of Córdoba. Campus de Rabanales, Edif. Leonardo da Vinci, 14071-Cordoba, Spain

Abstract. The study of baseflow in mountainous areas of basin headwaters, where the characteristics of the often fractured materials are very different to the standard issues concerning porous material applied in conventional hydrogeology, is an essential element in the characterization and quantification of water system resources. Their analysis through recession fragments provides information on the type of response of the sub-surface and subterranean systems and on the average relation between the storage and discharge of aquifers, starting from the joining of these fragments into a single curve, the Master Recession Curve (MRC). This paper presents the generation of the downward MRC over fragments selected after a preliminary analysis of the recession curves, using a hydrological model as the methodology for the identification and the characterization of quick sub-surface flows flowing through fractured materials. The hydrological calculation has identified recession fragments through surface runoff or snowmelt and those periods of intense evapotranspiration. The proposed methodology has been applied to three sub-basins belonging to a high altitude mountain basin in the Mediterranean area, with snow present every year, and their results were compared with those for the upward concatenation of the recession fragments. The results show the existence of two different responses, one quick (at the sub-surface, through the fractured material) and the other slow, with linear behaviour which takes place in periods of 10 and 17 days respectively and which is linked to the dimensions of the sub-basin. In addition, recesses belonging to the dry season have been selected in order to compare and validate the results corresponding to the study of recession fragments. The comparison, using these two methodologies, which differ in the time period selected, has allowed us to validate the results obtained for the slow flow.

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