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- W1539211047 abstract "A water balance of Sierras Blanca and Mijas Hydrogeological Unit, the most important aquifer in the Costa del Sol, in the period 1990/91-1993/94, has been made. The recharge is produced by the infiltration of rain water with a total amount of 116.9 hmhm 3 /year/year: 60.2 hm 3 /year has been evapotranspirated, 56.7 hm 3 /year belongs to the useful rain (8 hm 3 /year as streamflow and 48.7 hm /year as infiltration). The discharge have been measured and gives a total amount of 62.2 hm 3 /year: 28.2 hm 3 /year by the springs and 34 hm 3 /year by the pumpings. The useful rain has been calculated with several methods (Turc, Coutagne, Kessler, chloride method and monthly and daily Thornwaite method -with field capacities of 25 and 50 mm-). The method that fits in a better way with the known volumes of recharge and discharge, for each one of the aquifer system and for the whole Blanca-Mijas Hydrogeological Unit, is the chloride method." @default.
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- W1539211047 date "1997-04-30" @default.
- W1539211047 modified "2023-09-26" @default.
- W1539211047 doi "https://doi.org/10.3989/egeol.97531-2245" @default.
- W1539211047 hasPublicationYear "1997" @default.
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