Hydrogeochemical controls on groundwater salinization in a coastal aquifer, SE Ghana: Implications for seawater mixing and anthropogenic influences

IF 2.7 Q2 MULTIDISCIPLINARY SCIENCES
Shadrack Fosu , Felisa Maame Nuamah-Amonoo , Emmanuel Daanoba Sunkari , Emmanuel Abrokwah , Samuel Agyarko Ndur
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Abstract

Coastal aquifers across the globe are vulnerable to long-term salinization due to the attendant effects of climate change. Despite this threat to coastal aquifers, techniques for geochemical fingerprinting of the sources and factors controlling groundwater salinization are still evolving. Therefore, the purpose of this study was to assess the hydrogeochemical characteristics, identify sources of groundwater constituents, and evaluate processes and sources that contribute to groundwater salinization in the Ga West Municipality in SE Ghana by calculation of Revelle Index (RI) and Seawater Mixing Index (SMI) values, geochemical modelling, and chemometric analysis. The results indicate that sodium (Na+) and bicarbonate (HCO3-) are the dominant ions in the groundwater. The predominant water types are Na-HCO3-Cl (24.4 %) and Na-Ca-HCO3-Cl (17.2 %), with other mixed forms. The results of the chemometric analysis revealed that groundwater constituents are mainly derived from anthropogenic sources and salinization with limited contribution from geogenic and evaporation crystallisation processes. The groundwater shows undersaturation with respect to gypsum, calcite, aragonite, talc, halite, and quartz. The RI values range from 0.11 to 6.54 with an average value of 0.97, indicating that about 58.6 % of the boreholes in the study area are affected by salinization. Also, the SMI values indicate that 21 % of the samples show seawater intrusion as the cause of groundwater salinization. However, the groundwater salinization can also be attributed to anthropogenic activities like farming in the study area. These key findings imply that groundwater salinization in the Ga West Municipality driven by seawater mixing and human activities, poses a significant threat to agricultural productivity due to increased soil salinity. Thus, there is the need for sustainable groundwater management practices and monitoring systems to mitigate the impacts and ensure the availability of fresh water for future generations.
加纳东南部沿海含水层对地下水盐碱化的水文地球化学控制:对海水混合和人为影响的影响
由于气候变化的影响,全球沿海含水层很容易受到长期盐碱化的影响。尽管这对沿海含水层构成威胁,但控制地下水盐渍化的来源和因素的地球化学指纹技术仍在发展中。因此,本研究的目的是通过计算Revelle指数(RI)和海水混合指数(SMI)值,地球化学模拟和化学计量学分析,评估加纳东南部Ga West市的水文地球化学特征,确定地下水成分来源,并评价地下水盐渍化的过程和来源。结果表明,钠离子(Na+)和碳酸氢盐(HCO3-)是地下水中的主要离子。主要的水类型为Na-HCO3-Cl(24.4%)和Na-Ca-HCO3-Cl(17.2%),还有其他混合形式。化学计量学分析结果表明,地下水成分主要来源于人为来源和盐渍化,地质和蒸发结晶作用的贡献有限。地下水中石膏、方解石、文石、滑石、岩盐、石英等均呈欠饱和状态。RI值在0.11 ~ 6.54之间,平均值为0.97,表明研究区约58.6%的钻孔受到盐渍化的影响。此外,SMI值表明,21%的样品显示海水入侵是地下水盐渍化的原因。然而,地下水盐碱化也可归因于研究区农业等人为活动。这些关键发现表明,由于海水混合和人类活动的驱动,加西市地下水盐渍化由于土壤盐分增加而对农业生产力构成重大威胁。因此,需要可持续的地下水管理做法和监测系统,以减轻影响并确保为子孙后代提供淡水。
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来源期刊
Scientific African
Scientific African Multidisciplinary-Multidisciplinary
CiteScore
5.60
自引率
3.40%
发文量
332
审稿时长
10 weeks
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