2022
DOI: 10.1007/s13201-021-01559-2
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Characterization of groundwater in the 'Tamnean' Plutonic Suite aquifers using hydrogeochemical and multivariate statistical evidence: a study in the Garu-Tempane District, Upper East Region of Ghana

Abstract: The 'Tamnean' Plutonic Suite aquifer is the main public water supply for the Garu-Tempane District. Thus, hydrogeochemical characterization is essential to provide valuable insights into pollution sources and the main controls on groundwater chemistry. In this regard, multivariate statistical methods, conventional hydrochemical graphical methods, and various ionic ratios complemented with PHREEQC geochemical modelling were carried out using 38 groundwater samples collected from the Tamnean Plutonic Suite aquif… Show more

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Cited by 8 publications
(3 citation statements)
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References 68 publications
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“…The saturation index (SI) can be used to analyze the equilibrium state between groundwater and aquifer minerals during water-rock interaction [53]. The SI of calcite, dolomite, gypsum, and rock salt is calculated using Phreeqc 3.7.3, and the results are shown in Table 3.…”
Section: Saturation Index Analysismentioning
confidence: 99%
“…The saturation index (SI) can be used to analyze the equilibrium state between groundwater and aquifer minerals during water-rock interaction [53]. The SI of calcite, dolomite, gypsum, and rock salt is calculated using Phreeqc 3.7.3, and the results are shown in Table 3.…”
Section: Saturation Index Analysismentioning
confidence: 99%
“…Groundwater chemical composition involves the spatial and temporal variations due to precipitation, water-rock interaction, evaporation, redox reactions, recharge water quality, reactions of ion exchange, sorption, dissolution, climate, the grade of chemical weathering of different types of rock, mixing processes, etc. Hydrogeochemical analysis techniques in combination with stable isotope analysis (e.g., 18 O and 2 H), radioisotopes (e.g., 3 H and 14 C), and statistical techniques (e.g., Principal-Component-Analysis (PCA) and Hierarchical-Cluster-Analysis (HCA)) are often applied as effective methods to provide significant information regarding similarities among groundwater samples and/or hydrochemical variables, the groundwater residence times in aquifers, the source of groundwater in reservoirs, the groundwater movement's rate and direction, hydrochemical reactions in aquifers, climatic conditions during the recharge, hydraulic connection between different water sources, geological structure of aquifers, and anthropogenic impacts on aquifers (Zouari et al 2011;Fang 2019;Acikel and Ekmekci 2021;Okofo et al 2022;Zhao et al 2022;Nayak et al 2023;Ju et al 2024;Hamma et al 2024; amongst many others). These analysis techniques play a crucial role in enhancing our comprehension of hydrogeological systems.…”
Section: Introductionmentioning
confidence: 99%
“…The hydrogeochemical processes vary temporally and spatially depending on the chemical and geological characteristics of the aquifer. The residence time of the groundwater within the aquifer controls the groundwater chemical composition (Okofo et al, 2022). The major processes affecting the groundwater chemistry and quality are the rock-water interaction, especially dissolution and weathering processes, carbonate balance, oxidation-reduction, and adsorption-desorption, in addition to the anthropogenic activities and biochemical processes.…”
Section: Introductionmentioning
confidence: 99%