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Geo-chemical investigation of groundwater salinity status in selected coastal areas of south western Nigeria

机译:尼日利亚西南部选定沿海地区地下水盐度地质地理化学研究

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摘要

Groundwater remained main source of drinking water in Nigeria. Hydro-geochemical study was carried out to assess the influence of seawater on the chemical composition of groundwater in Badagry, Ikorordu, Epe, and Ondo Water side south western Nigeria. One hundred and ninety two (192) groundwater samples were collected from forty-eight (48) sampling points along the coastlines for four seasons (2015 through 2017). Analyses were carried out using standard procedures. Salinity-related parameters of the groundwater samples showed a range of 5.09-7.29 (pH), 1056-2249 μS/cm (electrical conductivity), 513.30-1439.30 mg/L (total dissolved solid), 43.15-2147 mg/L (alkalinity), 51.5-995. 5 mg/L (Cl~-), 2.75-11.75 mg/L (SO_4~(2-)), 8.78-32.11 mg/L (Na~+), 24.42-45.44 mg/L (K~+) 0.56-2.75 mg/L (Ca~(2+)), 0.09-5.55 mg/L (Mg~(2+)), and 7.2-39.15 mg/L (Hardness), respectively. Groundwater ionic characters were in order of HCO_3~- > Cl~- > SO_4~(2-) for anions and K~+> Na~+ > Ca~+ > Mg~(2+) for cations. Though concentration of bicarbonate was high as expected of inland water, salinity-related parameters were above the acceptable limits. Results revealed that the groundwater samples in the areas have saline water signatory probably as a result of prevailing climate influence (sea-level rise and flooding) which predisposes the users to diverse infections and other cardiovascular diseases associated with intake of saltwater. Water quality index also showed that groundwater in the areas are contaminated and unfit for human consumption. Achieving water sustainability in the area would demand appropriate water safety plan and proper water treatment.
机译:地下水仍然是尼日利亚饮用水的主要来源。进行了水力地球化学研究,以评估海水对巴斯塔德,Ikorordu,EPE和Ondo水侧西南部地下水化学成分的影响。从四季到四季(2015到2017)的海岸线的四十八(48)个采样点收集了一百九十二(192)个地下水样品。使用标准程序进行分析。地下水样品的盐度相关参数显示为5.09-7.29(pH),1056-2249μs/ cm(电导率),513.30-1439.30 mg / L(总溶解固体),43.15-2147mg / l(碱度),51.5-995。 5 mg / L(Cl〜 - ),2.75-11.75 mg / L(SO_4〜(2-)),8.78-32.11 mg / L(Na〜+),24.42-45.44 mg / L(K〜+)0.56- 2.75mg / L(Ca〜(2+)),0.09-5.55mg / L(Mg〜(2+))和7.2-39.15 mg / L(硬度)。用于阴离子的HCO_3〜 - > Cl〜 - > SO_4〜(2-)的地下水离子特征是阳离子的阴离子和K〜+> Na〜+> Ca〜+> Mg〜(2+)。虽然碳酸氢盐的浓度高于内陆水的预期高,但盐度相关参数高于可接受的限度。结果表明,该地区的地下水样品可能是盐水签字,可能是普遍存在的气候影响(海平面上升和洪水),这使得用户倾向于不同于与盐水的摄入相关的感染和其他心血管疾病。水质指数还表明,该地区的地下水受到污染,不适合人类消费。在该地区实现水可持续性将需要适当的水安全计划和适当的水处理。

著录项

  • 来源
    《Sustainable Water Resources Management》 |2021年第4期|62.1-62.15|共15页
  • 作者单位

    Department of Water Resources Management and Agro-Meteorology Federal University Oye-Ekiti Oye Ekiti Nigeria;

    Department of Physics Federal University of Agriculture Abeokuta Ogun Nigeria;

    Department of Water Resources and Agro-Meteorology Federal University of Agriculture Abeokuta Nigeria;

    Department of Environmental Management and Toxicology Federal University of Agriculture Abeokuta Ogun Nigeria;

    Department of Geography and Planning Science Faculty of The Social Sciences Ekiti State University Ado Ekiti Nigeria;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Groundwater; Salinity; Concentration; Climate;

    机译:地下水;盐度;专注;气候;

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