Contribución al contenido en tritio a la identificación del origen del agua subterránea: Sierra de Gador (Almería).

  1. Vallejos Izquierdo, Ángela
  2. Pulido Bosch, Antonio
  3. Molina Sánchez, Luis
  4. Sánchez Martos, Francisco
  5. Gisbert, Juan
  6. Martín Rosales, Wenceslao
Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 2001

Número: 31

Páginas: 83-86

Tipo: Artículo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

Resumen

Tritium content of rainwater in Sierra de Gador has been higher than at. 10 TU during the last forty years. Groundwater samples apparently indicate the absence of recent contributions from the precipitation. The mixture with older waters stored inside the aquifer frequently hides the presence of modem recharge. From the content in tritium one can recognize two areas of preferential flow and recharge. One coincides with vulnerable basins to the generation of surface runoff and the other one is bound to a process of marine intrusion

Fuente de los datos: Dialnet