Hydrogeological and geophysical investigation of the salinization in the Martil Coastal aquifer (Tetouan-Morocco)
Lamrini, A.; Beeuwsaert, E.; Walraevens, K. (1999). Hydrogeological and geophysical investigation of the salinization in the Martil Coastal aquifer (Tetouan-Morocco). Natuurwet. Tijdschr. 79(1-4): 215-219
In: Natuurwetenschappelijk Tijdschrift. L. Walschot/Natuur- en Geneeskundige Vennootschap: Gent. ISSN 0770-1748, meer
Ook verschenen 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. 307 pp., meer
The Martil-Allila plain is a part of the series of alluvial plains of the Moroccan Rifs Mediterranean border. Alluvial terraces constituted by gravel, sand, silt and clay form it. In spite of the lithological variability, the analysis of borehole data has revealed the typical lithological structure of the plain. The interpretation of geoelectrical soundings, supported by results obtained from hydrochemical and hydrogeological observations, has shown the presence of an unconfined aquifer with brackish salt water, separated by an aquitard from a confined aquifer containing fresh water.
Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid
