Evolución del contacto agua dulce-agua salada en un acuífero kárstico costeroacuífero de Aguadulce (Almería)

1. Sánchez Martos, Francisco
2. Gisbert, Juan
3. Pulido Bosch, Antonio
4. Vallejos Izquierdo, Ángela
5. Molina Sánchez, Luis

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lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

Resumen

Karstic aquifers display a large number of singularities regarding the underground flow organisation and the vertical distribution of the water heads, due to the unequal behaviour of the karstic drains and channels compared to the matrix. In the coastal aquifers, the existence of a saltwater and a mixing zone, whose dynamics may turn very complicated, must be added to the usual complexity. The monitoring of the piezometric level and electrical conductivity evolution in a borehole in the Campo de Dalias aquifer allow the exposition of a series of considerations about the evolution of the measured parameters and the factors that determine this evolution.

Fuente de los datos: Dialnet