|The fresh-/salt-water flow and distribution in a cross-section through the dunes of Saidia Plain (north-eastern Morocco)|
El Halimi, N.; Chaouni Alia, A.; Lebbe, L.; Beeuwsaert, E.; Walraevens, K. (1999). The fresh-/salt-water flow and distribution in a cross-section through the dunes of Saidia Plain (north-eastern Morocco), in: De Breuck, W. et al. (Ed.) Proceedings of the 15th Salt-Water Intrusion Meeting Ghent (Belgium), 25-29 May 1998. Natuurwetenschappelijk Tijdschrift, 79(1-4): pp. 205-211
In: De Breuck, W.; Walschot, L. (Ed.) (1999). Proceedings of the 15th Salt-Water Intrusion Meeting Ghent (Belgium), 25-29 May 1998. Natuurwetenschappelijk Tijdschrift, 79(1-4). Natuurwetenschappelijk Tijdschrift: Gent, Belgium. 307 pp., more
In: Natuurwetenschappelijk Tijdschrift. L. Walschot/Natuur- en Geneeskundige Vennootschap: Gent. ISSN 0770-1748, more
|Available in|| Authors |
VLIZ: Proceedings D 
|Document type: Conference paper|
Dunes; Fresh water; Ground water; Mathematical models; Saline water; MED, Morocco [Marine Regions]
|Authors|| || Top |
- El Halimi, N.
- Chaouni Alia, A.
- Lebbe, L., more
- Beeuwsaert, E.
- Walraevens, K., more
The unconfined aquifer in the coastal plain of Saidia (north-eastern Morocco) is characterized by the presence of salt water. It is composed of unconsolidated Quaternary deposits reaching levels down to -10 to -22 m. Its substratum is constituted by clay or marly clay of Miocene age. Borings with resistivity logging have provided information about the lateral and vertical distribution of groundwater quality. A freshening of groundwater is observed, mainly resulting from recharge in both dune belts. The evolution of the fresh- and salt-water flow and distribution has been modelled in a cross-section by means of a mathematical model, taking the resistivity loggings into account. This cross-section is perpendicular to the shoreline.