Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon

• Published in: Discover water 2023-07, Vol.3 (1), p.10-13, Article 10
• Main Authors: Menti, Agbor Nelson, Wotany, Egome Regina, Christopher, Agyingi, Wirmvem, Menjo Jude, Ngai, Nfor Jude
• Format: Article
• Language: English
• Subjects: Alkalinity; Aquatic Pollution; Aquifers; Bertoua Cameroon; Coastal Sciences; Earth and Environmental Science; Earth Sciences; Geology; Groundwater; Groundwater quality; Hydrogeochemistry; Hydrogeology; Ion exchange; Marine & Freshwater Sciences; Oceanography; Pan-Africanism; Silicate weathering; Surface water; Temperature; Testing laboratories; Waste Water Technology; Water Management; Water Pollution Control; Water quality; Water supply
• ISSN: 2730-647X; 2730-647X
• DOI: 10.1007/s43832-023-00034-0

Groundwater and surface water are major sources of water supply to the inhabitants of Bertoua. Hydrogeochemical study conducted in the study area aimed at identifying the processes that control the chemistry of groundwater sources and to examine the quality of the water sources for domestic and agricultural purposes. Fifty water samples were collected from boreholes, open wells, springs, and rivers within the study area in January 2022 (the dry season). The samples were analyzed for physicochemical characteristics including pH, electrical conductivity (EC), total dissolved solids (TDS) and major ions. The water samples were acidic with 94% of pH values less than 6.5. The EC varied from 21 to 776 µS/cm and TDS (8.5–388 mg/l). The low EC and TDS indicate low mineralization and fresh water. The relative abundance of major ions (meg/l) was Ca 2+ > Mg 2+ > K + >Na + for cations and HCO 3 - >Cl − >NO 3 − >SO 4 2− for anions. These major ions concentrations were low and within the WHO guideline values for drinking water. From Piper diagram three water facies were observed; Ca-SO 4 , Ca-HCO 3 and mixed Ca-Mg-Cl. Rock-water interaction, ion exchange, silicate weathering and anthropogenic activities were the processes responsible for the groundwater chemistry with some minor evaporative effects. Based on Sodium Adsorption Ratio and Residual Sodium Bicarbonate all samples fall in the excellent category for agriculture.