Primeros resultados acerca de la interacción entre aguas subterráneas y superficiales en La Charca de Suárez (Granada)
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Abstract
La Reserva Natural Concertada de La Charca de Suárez es un
humedal costero situado al sur de España. El complejo lagunar comprende 8 lagunas que se encuentran en zonas ligeramente deprimidas del acuífero Motril-Salobreña, donde el nivel freático intersecta
la topografía. La hidrodinámica del sistema fue analizada en 4 de
las 8 lagunas mediante el análisis de datos de elevación de nivel
piezométrico, descarga de agua subterránea medida con exfiltrómetros, flujos superficiales y condiciones climáticas. Los resultados
muestran diferencias en la interacción con el agua subterránea para
cada una de las lagunas. Además, se pueden observar cambios estacionales y eventuales que indican la necesidad de un seguimiento
continuo de la red de control en el humedad
The Charca de Suárez Nature Reserve is a coastal wetland located in the south of Spain. The wetland complex is composed of 8 lakes in a lowland area of the Motril-Salobreña aquifer, where the watertable is near to the surface topography. The hydrodynamic of this system was analyzed in 4 of the 8 lagoons based on water table elevation, seepage meter measurements, surficial flow and climatic conditions. The results showed differences in the interaction with groundwater for each of the lakes conforming the wetland. Also, seasonal and event related changes can be observed, which indicates the necessity of continuous measurements in the wetland
The Charca de Suárez Nature Reserve is a coastal wetland located in the south of Spain. The wetland complex is composed of 8 lakes in a lowland area of the Motril-Salobreña aquifer, where the watertable is near to the surface topography. The hydrodynamic of this system was analyzed in 4 of the 8 lagoons based on water table elevation, seepage meter measurements, surficial flow and climatic conditions. The results showed differences in the interaction with groundwater for each of the lakes conforming the wetland. Also, seasonal and event related changes can be observed, which indicates the necessity of continuous measurements in the wetland







