Caracterización hidroquímica de las relaciones río-acuífero en la Sierra de Lújar (Granada)

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