Abstract
Tadla Plain is one of the most water-productive areas of the central Moroccan and also a fertile tract for agriculture. Our study is concerned with the Dir (Piedmont) aquifer in the sub-urban area of Beni Mellal. The aims of this paper are: (i) to identify some of the main hydrochemical processes controlling groundwater chemistry under the city of Beni Mellal and the impact of urban activities, (ii) to detect and understand the spatial variations of the occurring hydrochemical processes in order to localize areas with the most noticeably contaminated groundwater, (iii) to know the groundwater suitability for drinking, irrigation, and industrial purposes. Fifty-one groundwater samples during spring 2014 were collected and analyzed for physical and chemical groundwater parameters (electrical conductivity EC, pH, total dissolved solid TDS, T°, NO3−, SO42−, HCO3−, Cl−, Na+, K+, Ca2+, Mg2+, and trace elements such as Ba, Li, Fe, Mg, Al, Cd, Cr, Cu, Mn, Ni, Pb and Zn). The overall hydrochemistry reflects rock weathering with impregnation of anthropogenic impacts due to the urbanization and agricultural manures. The electric conductivity and the total dissolved solids have values more than the desirable limit of 750 µS/cm and 500 mg/l respectively in 49 and 59% of the total groundwater samples. The concentration of light metal does not exceed the recommended threshold with the following order Ca2+ > Mg2+ > Na+ > K+. Bicarbonate, nitrates, and chloride show contents under the desired guidelines contrary to the content of sulfate, which exceeds the threshold of Moroccan guidelines especially in the central city zone. The abundance of anions is in the following order: HCO3− > SO42− > Cl− > NO3−. The main hydrogeochemical process is dissolution and weathering from parent rock and cation–cation exchange. All calculated parameter indexes are in concordance that Beni Mellal groundwater is excellent to good for irrigation purposes. The CaCO3 supersaturation restricts the safe use of water for industrial purpose. For most of the trace elements, the measured concentrations were far below the standard values except Al and Fe in some samples, which exceed all guideline values. The use of PCA allowed extracting four principal components (F) using a Kaiser criterion and varimax rotated method, which explained 60% of the total variance. The highest F1 scores are concentrated in the central area, indicating a higher degree of water–rock interactions supplying elements with higher mobility to groundwater. Also, concentrated mobile elements can be reported on more anthropic activities. F2 scores showed a more scattered distribution compared to F1 scores with a concentration around peripheral zones of the city.
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Notes
ONEE, Office National de l’Electricité et de l’Eau potable.
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Acknowledgements
This research has been carried out as part of research that was partly funded by the University Sultan Moulay Slimane. We are thankful to Prof. B. Mernari, President of the University for his support and for providing the working facilities. The Director of ONEE of Beni Mellal (Branche Eau) is thanked for providing the water laboratory of Ain Asserdoune for titrimetric analysis. The authors are also thankful to Hind Nassri for their help in the field and analytical laboratory work.
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This paper has been selected from the 1st Euro-Mediterranean Conference for Environmental Integration, Tunisia 2017.
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El Baghdadi, M., Zantar, I., Jouider, A. et al. Evaluation of hydrogeochemical quality parameters of groundwater under urban activities—Case of Beni Mellal city (Morocco). Euro-Mediterr J Environ Integr 4, 6 (2019). https://doi.org/10.1007/s41207-018-0087-4
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DOI: https://doi.org/10.1007/s41207-018-0087-4