Origin of spring water chemistry and its appropriateness for drinking requirements in a semi-arid environment (Ain Larbi, Algeria)

Abstract

A comparative assessment of water quality for drinking purposes was conducted in Ain Larbi area using the Weighted Arithmetic Water Quality Index (WA-WQI). The origin of minerals is assessed by a saturation index approach and the Gibbs diagram. Also, mineral correlation process and ion exchange mechanism are detected by the Principal Component Analysis (PCA). The PCA results indicate that the groundwater quality in the Ain Larbi study area primarily results from weathering and geochemical alteration of rock. The saturation index and Gibbs diagram support these findings. The WA-WQI was calculated for each station based on physicochemical parameters. During the wet season, three out of five classes of WQI were observed in the present study, including excellent (25%), good (70%), and poor (5%). In the dry season, the classes excellent (25%), good (30%), and poor (45%) were represented. The present situation demonstrates how hydrogeological regimes and water–rock interactions affect groundwater ion concentrations. Our results contribute to identifying drinking water requirements in the Ain Larbi region, promoting sustainable water management. HIGHLIGHTS Hydro-chemical facies for discerning the diverse nature of water.; The origin of water minerals and the geochemical processes.; Mineral correlation process and ion exchange mechanism.; Calculation for assessing the qualities of drinking water.; Water assessment in a semi-arid area.; Detecting a potential pollution.;

Keywords

• ain larbi springs
• mineralization process
• physicochemical composition
• water quality
• wa-wqi