Published 1996 | Version v1
Miscellaneous

Isotopic, hydrochemical, and hydrogeological study of deep aquifer of Sfax: First results

  • 1. Laboratoire de geochimie isotopique et de paleoclimatologie, ecole nationale d'ingenieurs de Sfax, (Tunisia)
  • 2. Direction des ressources en eaux, CRDA de Sfax, (Tunisia)

Description

The water of the chlorinated sodic with chemical facies deep aquifer of Sfax presents a difference on the level of mineralization between the northern sector with a relatively weak salin charge (average of 3,5 g/l) and the southern sector with an important mineralization (about 10g/l). The mineralization of water in linked to dissolution phenomena. Based on the first isotopic results, it seems that the present refill of the deep aquifer of Sfax is very weak (author)

Part of:
Proceedings of the international colloque on the use of isotopic techniques in water and soil resources field

Additional details

Additional titles

Original title (French)
Etude hydrogeologique, hydrochimique et isotopique de la nappe profonde de Sfax : premiers resultats

Publishing Information

Imprint Title
Proceedings of the international colloque on the use of isotopic techniques in water and soil resources field
Imprint Pagination
104 p.
Journal Page Range
p. 41-47

Conference

Title
International colloque on the use of isotopic techniques in water and soil resources field
Dates
13-15 Jun 1996
Place
Mahdia (Tunisia)

Optional Information

Notes
8 refs. Imprint:Actes du colloque international sur l'utilisation des techniques isotopiques dans le domaine des ressources en eau et en sol