Abstract

The M’zab region is subject to an arid Saharan climate where surface and sub-surface waters are of little importance. The Albian Aquifer, commonly called Continental Intercalary (CI), main component of North Western Sahara Aquifer System (NWSAS/SASS), constitutes the most extensive aquifer formation of the region. In our study area, the CI is identified, as a regional subset, as the Albian Aquifer of M’zab Region (AAMR). Its groundwater resources are considered the only source available to meet the growing needs of drinking water supply, agriculture and industry. This aquifer is heavily exploited by a very large number of wells (more than 750). Its supply is very low, so it is a very low renewable layer. This requires periodic monitoring and control of its piezometric level and its physico- chemical quality. The objective of our study is to know the current state of this aquifer, while studying the variation of its piezometry for the period 2010-2018, and also the chemical quality of its groundwater by analyzing more than 90 samples over the entire study area. The application of geostatistics by kriging and the steps of analysis, modelling and calculation of semivariogram have enabled us to draw up maps of the various hydrogeological and hydrochemical parameters. As a result, twelve thematic maps were gridded using Geostatistical tools of ArcGIS software. The water-level-change map showed a significant drop in the groundwater level over the entire M’zab region and especially around the major cities (Ghardaïa, Berriane, Metlili and Zelfana) with more than 8 meters. Chemical analyses of the Albian groundwater in the study area show the dominance of evaporite facies (Cl--Na+-Ca2+) with low concentrations than the Algerian Standards for Drinking (ASD). All the water quality indices (WQI) that have been mapped reveal that the groundwater samples were suitable for drinking and irrigation with a high quality of water located in the south of the study area.

Highlights

  • In the Algerian Sahara known for its arid climate, groundwater is the main source of water used mainly for domestic and irrigation practices in the area [1]

  • The piezometric maps that have been obtained (2010 and 2018) (Figure 4, Figure 5) confirm very clearly the general flow directions of the continental intercalary aquifer which is already known in the entire northern Sahara basin North-Est and North-Southwest

  • The piezometry of the Albian Aquifer of M’zab Region (AAMR) shows depressions located in urban centers and agricultural areas in our study area

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Summary

Introduction

In the Algerian Sahara known for its arid climate, groundwater is the main source of water used mainly for domestic and irrigation practices in the area [1]. There has been a significant increase in water demand due to local population growth and agricultural development. Under these conditions, aquifers are in a situation of over-exploitation with pumped volumes far exceeding natural recharge rates [2]. Its waters are the main water resources used in the region. It is exploited by more than 750 water wells with a volume of 531.76 Hm3 [3]. One of the effects is the localized deterioration of the chemical quality of the groundwater

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