Caracterización hidroquímica de las relaciones río-acuífero en la Sierra de Lújar (Granada)
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Abstract
Besides of the early-summer snowmelt effect on the Guadalfeo river salinity, the hydrochemical data point out that a significant part of the discharge of the Sierra de Lújar carbonate aquifer is made directly towards the Guadalfeo alluvium, and the springs seem to drain a fraction-perhaps only minor of the whole groundwater resources







