La remontre des eaux souterraines en surface: mecanisme et l'impact sur l'environnement (cas de Oued Souf). Magister thesis (2011), Université de Batna 2.
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Date
2017-04-11
Authors
ZINE Brahim
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Abstract
The area of Oued Souf has been confronted with the phenomenon of the upwelling of water for several years and without almost any cease to become more extensive each year. This phenomenon took very alarming dimensions the last twenty years. The use of the deep layers water (the Continental intercalary and the Final Complex) in an excessive way considerably increased the volume of the water input, as well as the absence of a natural discharge system for the rejections of wastewater, are the principal causes of this ecological imbalance. Contributing to the deterioration of the palm trees, the inundation of (Ghouts) causes mortal consequences at the level of environment, agriculture, the economy and the health of Oued Souf area. Piezometry revealed that groundwater zone upwelling, corresponds to piezometric depressions which led to water accumulation, especially wastewater. Water chemistry has complied with the above hypothesis in reference to the fact that waters have a very poor quality at this level.