“…This indicates that the magnesium, sodium, and bicarbonate ions are positively charged. Weathering of silicate and carbonate minerals, dissolved minerals in sedimentary rocks, and leaching from the soil surface during rainstorms were all possible sources of ionic concentrations for the first component (PC1) ( Egbueri et al., 2022 ; Nguyen et al., 2020 ). PC1 also has medium loading scores for EC, TH, TDS, Ca 2+ , SO 4 2− , and Cl − .…”