Geochemical and qualitative assessment of groundwater of the High Mekerra watershed,NW Algeria |
| |
| Authors: | Bachir Hallouche Abbas Marok Lahcen Benaabidate Yagoubia Berrahal Fatiha Hadji |
| |
| Affiliation: | 1.Department of Civil Engineering,University of Djillali Liabes,Sidi Bel Abbes,Algeria;2.Department of Earth and Universe Sciences,University of Tlemcen,Tlemcen,Algeria;3.Laboratory of Georesources and Environment, Faculty of Sciences and Technology,Fez,Morocco;4.Department of Chemistry,University of Djillali Liabes,Sidi Bel Abbes,Algeria |
| |
| Abstract: | Groundwater constitutes the main source of water supply in the High Mekerra watershed of northwestern Algeria. This resource is currently under heavy pressures to meet the growing needs of drinking water and irrigation. This study assesses the geochemical characteristics of groundwater of the High Mekerra watershed at 21 points distributed across the two main aquifers (Ras El Ma and Mouley Slissen) in the region. Hydrochemical facies of Ras El Ma groundwater are dominantly MgCl and CaCl type, while those of Mouley Slissen groundwater are of CaHCO3 type. Principal component analysis shows a strong correlation between groundwater mineralization and Ca2+, Na+, Cl? and SO4 2? ions stemming from the dissolution of carbonates, gypsum and anhydrite. Groundwater mineralization evolves from south to north. Geochemical modeling shows that the High Mekerra groundwater is saturated with respect to calcite and dolomite and undersaturated with respect to gypsum and anhydrite. Nitrate concentrations that exceed the WHO standard (50 mg L?1) at several points are linked to the agro-pastoral activities in this region. |
| |
| Keywords: | |
| 本文献已被 SpringerLink 等数据库收录！ |
|
