Loading...
Please wait, while we are loading the content...
Similar Documents
Détermination des modalités de recharge des aquifères par le biais des traceurs chimiques et isotopiques. Cas de la zone de contact Haut Atlas occidental – Plaine du Souss (SW du Maroc)
| Content Provider | Semantic Scholar |
|---|---|
| Author | Boutaleb, Said Bouchaou, Lhoussaine Hsissou, Y. Tagma, Tarik |
| Copyright Year | 2008 |
| Abstract | Determination of the origin of recharge of the unconfined aquifer in the right side of the Souss wadi between Agadir and Taroudant (South-western of Morocco) was based on the use of hydrochemical and isotopic analysis of groundwater, surface water and springs of the contact zone between the High-Atlas Chain and the Souss plain. The correspondence in the space evolution of the various chemical elements of evaporitic origin (SO 4 2- , Cl - , Sr 2+ ) in groundwater, piedmont springs, and surface water reveals the existence of recharge water from the adjacent High-Atlas Chain. The various recharge modes of the different aquifers (High Atlas and Souss plain) determined by isotopic analysis, shows that the source of groundwater for the unconfined Souss aquifer seems to be composite between a direct infiltration on the High-Atlas tributaries and a remote recharge from the bordering High Atlas aquifers. |
| Starting Page | 45 |
| Ending Page | 60 |
| Page Count | 16 |
| File Format | PDF HTM / HTML |
| DOI | 10.3989/egeol.08641459 |
| Volume Number | 64 |
| Alternate Webpage(s) | http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/download/459/481 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
