| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5445098 | Energy Procedia | 2017 | 11 Pages |
Abstract
The followed hydrochemical of the five sources showed the same chemical facies which is calcic to magnesian bicarbonated with predominance of the first facies; except the source of Ain Sari is composed of calcic chlorinated. The evolution of the contents of the chemical elements is due to the increase in the flow of the sources after the period of flood which demonstrates the effect of the behavior of the karst area.
Keywords
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Physical Sciences and Engineering
Energy
Energy (General)
Authors
Radhia Legrioui, Fethi Baali, Amor Hamad, Ilhem Abdeslam, Mouici Redha,