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Evolution of the fresh water-saltwater contact in a karstic coastal aquifer: Aquifer of Aguadulce (Almería)

dc.contributor.authorVallejos, Ángela
dc.contributor.authorPulido Bosch, Antonio
dc.contributor.authorGisbert, Josep
dc.contributor.authorSánchez Martos, Francisco
dc.contributor.authorMolina, Luis
dc.description.abstractKarstic 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 evolutionen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherKarstic aquiferen_US
dc.subject.otherPiezometric levelen_US
dc.titleEvolución del contacto agua dulce-agua salada en un acuífero kárstico costero: acuífero de Aguadulce (Almería)en_US
dc.titleEvolution of the fresh water-saltwater contact in a karstic coastal aquifer: Aquifer of Aguadulce (Almería)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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