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

Abstract 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...

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Main Authors: Agbor Nelson Menti, Egome Regina Wotany, Agyingi Christopher, Menjo Jude Wirmvem, Nfor Jude Ngai
Format: Article
Language:English
Published: Springer 2023-07-01
Series:Discover Water
Subjects:
Online Access:https://doi.org/10.1007/s43832-023-00034-0
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author Agbor Nelson Menti
Egome Regina Wotany
Agyingi Christopher
Menjo Jude Wirmvem
Nfor Jude Ngai
author_facet Agbor Nelson Menti
Egome Regina Wotany
Agyingi Christopher
Menjo Jude Wirmvem
Nfor Jude Ngai
author_sort Agbor Nelson Menti
collection DOAJ
description Abstract 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 Ca2+> Mg2+> K+>Na+ for cations and $${\text{H}\text{C}\text{O}}_{3}^{-}$$ HCO 3 - >Cl−>NO3 −>SO4 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-SO4, Ca-HCO3 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.
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spelling doaj.art-1479ca1f63b94b518c59c6e26b4d30ff2023-07-16T11:27:25ZengSpringerDiscover Water2730-647X2023-07-013111310.1007/s43832-023-00034-0Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-CameroonAgbor Nelson Menti0Egome Regina Wotany1Agyingi Christopher2Menjo Jude Wirmvem3Nfor Jude Ngai4Department of Geology, Faculty of Science, University of BueaDepartment of Geology, Faculty of Science, University of BueaDepartment of Geology, Faculty of Science, University of BueaInstitute of Geological and Mining ResearchInstitute of Geological and Mining ResearchAbstract 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 Ca2+> Mg2+> K+>Na+ for cations and $${\text{H}\text{C}\text{O}}_{3}^{-}$$ HCO 3 - >Cl−>NO3 −>SO4 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-SO4, Ca-HCO3 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.https://doi.org/10.1007/s43832-023-00034-0HydrogeochemistryIon exchangeSilicate weatheringGroundwater qualityBertoua Cameroon
spellingShingle Agbor Nelson Menti
Egome Regina Wotany
Agyingi Christopher
Menjo Jude Wirmvem
Nfor Jude Ngai
Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon
Discover Water
Hydrogeochemistry
Ion exchange
Silicate weathering
Groundwater quality
Bertoua Cameroon
title Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon
title_full Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon
title_fullStr Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon
title_full_unstemmed Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon
title_short Hydrogeochemical characterization of ground and surface water in the eastern part of the Adamawa-Yade domain, Bertoua-Cameroon
title_sort hydrogeochemical characterization of ground and surface water in the eastern part of the adamawa yade domain bertoua cameroon
topic Hydrogeochemistry
Ion exchange
Silicate weathering
Groundwater quality
Bertoua Cameroon
url https://doi.org/10.1007/s43832-023-00034-0
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