The Continental intercalary groundwater is highly sought for its water as resources hugely mobilized in Northern Sahara. A very high flow rate and output pressure characterizes this underground water. It amounts from 50 to 400 l.s-1 for the flow, and from 5 to 40 bar for pressure. A survey of the Northern Sahara Aquifer System was essential to prove the existence of this potential. This energy appears into the artesian form, which remains very considerable for a very long time in most drilling. We have realised that this energy is immense, as well as the expanded volume of the groundwater, and the importance of its use in agriculture. Unfortunately, this potential remains untapped to this day and the energy of this water is completely negle...
Texte intégral accessible uniquement aux membres de l'Université de LorraineThe eastern plain of ann...
Inféro-flux phreatic aquifer (Biskra, NE Algeria) is overexploited for irrigation and drinking water...
This study assesses mechanisms responsible for the aquifer salinization in the Guerrara oasis, in so...
AbstractThe Intercalary Continental aquifer generally called Albian aquifer constitutes the main geo...
The Intercalary Continental aquifer generally called Albian aquifer constitutes the main geothermal ...
AbstractThe Algerian Sahara contains important potential underground water. These resources, which w...
The study area is one of the important geothermal provinces in south Algeria. It is characterized by...
The M’zab valley is a hyper arid region of average rainfall not exceeding 100 mm per year. However, ...
The question of water resources is posed urgently in Algeria. Underground water resources have been ...
[EN] The aim of this work is the exploration of groundwater resources in the southeastern corner of...
Groundwater resources in semi-arid areas and especially in the Mediterranean face a growing demand f...
North Africa arid regions of Maghreb suffers of dry climatic conditions with erratic behaviour of ra...
El Outaya plain is located on the southern flank of the Aures Mountains, as part of ??the Saharan At...
Numerical simulation of the aquifer of Annaba (Salines zone -Eastern Algeria). The hydrogeological s...
Exploitation of karstic aquifers in Algeria Somes difficulties are specific of the karstic aquifers...
Texte intégral accessible uniquement aux membres de l'Université de LorraineThe eastern plain of ann...
Inféro-flux phreatic aquifer (Biskra, NE Algeria) is overexploited for irrigation and drinking water...
This study assesses mechanisms responsible for the aquifer salinization in the Guerrara oasis, in so...
AbstractThe Intercalary Continental aquifer generally called Albian aquifer constitutes the main geo...
The Intercalary Continental aquifer generally called Albian aquifer constitutes the main geothermal ...
AbstractThe Algerian Sahara contains important potential underground water. These resources, which w...
The study area is one of the important geothermal provinces in south Algeria. It is characterized by...
The M’zab valley is a hyper arid region of average rainfall not exceeding 100 mm per year. However, ...
The question of water resources is posed urgently in Algeria. Underground water resources have been ...
[EN] The aim of this work is the exploration of groundwater resources in the southeastern corner of...
Groundwater resources in semi-arid areas and especially in the Mediterranean face a growing demand f...
North Africa arid regions of Maghreb suffers of dry climatic conditions with erratic behaviour of ra...
El Outaya plain is located on the southern flank of the Aures Mountains, as part of ??the Saharan At...
Numerical simulation of the aquifer of Annaba (Salines zone -Eastern Algeria). The hydrogeological s...
Exploitation of karstic aquifers in Algeria Somes difficulties are specific of the karstic aquifers...
Texte intégral accessible uniquement aux membres de l'Université de LorraineThe eastern plain of ann...
Inféro-flux phreatic aquifer (Biskra, NE Algeria) is overexploited for irrigation and drinking water...
This study assesses mechanisms responsible for the aquifer salinization in the Guerrara oasis, in so...