Abstract
The chemical characterization of the Ghis-Nekor groundwater has become a concern of many researchers in Morocco. It is a crucial indicator for the environment situation and the socioeconomic development of this Moroccan region. Indeed, it helps decisionmakers carry out conscious and sustainable management. For this reason, 20 samples of the Ghis-Nekor aquifer were examined in terms of physicochemical parameters such as pH, temperature, electrical conductivity (EC), and total alkalinity (Alk), major cations–anions (Ca2+, Mg2+, Na+, K+, HCO3−, Cl−, SO42−, NO3−, and TDS), isotopic elements (δ18O, δ2H, and δ13C), and concentrations of Br and Sr anions in 2020. Furthermore, spatial data analysis with a geographic information system (GIS) using the ArcGis software (Redlands, California, USA). Indeed, static maps show significant water quality information that helps characterize the groundwater of the study area. The spatial analysis by the GIS indicates that except the EC (from 2630 to 6950 mS/cm), all the physical parameters showed standard concentration values in most of the samples. A significant concentration above the Moroccan norm of groundwater quality for sodium (Na+) from 264.3 to 1500 mg/L, chlorides (Cl−) concentrations from 408.3 to 1510 mg/L, SO42− from 313.1 to 999.2 mg/L, and bicarbonate (HCO3−) from 283.7 to 679.8 mg/L was observed, while all the points exceeded the recommended standards norm for SO42−. Most of the points met the potability standards for potassium (K+). In terms of the isotopic elements, the concentration values of δ18O were from −3.92‰ to –5.60‰, while the δ2H concentration values varied between −28.67‰ and −39.99‰. The analysis revealed values of carbon isotope δ13C ranging between −3.15‰ and −8.61‰, thus suggesting that the origin of the carbon is mineral, mainly deriving from calcite dissolution. The analysis of the bromide and strontium contents made it possible to discriminate the origin of the salinity anomalies. The Cl/Br, Br/Cl, and Sr/Ca molar ratios distinguished the areas of influence of geological setting (saliferous facies outcrops) or anthropogenic effect (wastewater). The results of the analysis shed light on factors of contamination, which are as follows: urban zones (Imzourene, Ait Youssef, and Souani) and agricultural activities. Therefore, the use of these waters could pose a risk to the health of humans and animals. Similarly, the GIS is a practical and effective tool for the Ghis-Nekor groundwater quality diagnostics and could help decisionmakers establish solutions.
Highlights
In Morocco and other dry countries, water is a limited resource that needs optimal strategies of management and protection against all types of pollution [1]
The hydrochemistry of the groundwater is characterized using static maps elaborated by the geographic information system (GIS) geostatistics module
The analysis of the results revealed that groundwater samples have temperatures between 18.78 ◦ C (P19) and 23.07 ◦ C (P9), with an average of 21.6 ◦ C (Table 1)
Summary
In Morocco and other dry countries, water is a limited resource that needs optimal strategies of management and protection against all types of pollution [1]. The GhisNekor alluvial aquifer is one of the most important aquifers in the northeast of the Loukkos hydrological basin, in the north of Morocco. It plays a strategic role in the drinking water supply of the surrounding major cities and urban centers, and in the irrigation supply as well. Its importance triggered a huge body of research that investigated the aquifer in many aspects. Salhi [2] studied the Ghis-Nekor aquifer extensively and provided a reference for the following studies. El Asri et al [7] simulated the climate change impact following different projections on groundwater recharge in the region
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