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Assessment of groundwater potential and quality using geophysical and physicochemical methods in the basement terrain of Southwestern, Nigeria

机译:利用西南地区地球物理化学方法评估地下水潜力和质量

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An integrated approach involving geophysical and physicochemical methods was undertaken to assess the potential availability of groundwater and its quality was carried out at Akole, Abeokuta Southwestern Nigeria. A combination of electrical resistivity and natural electric field methods were used in delineating the sub-surface lithology, determining potential groundwater-bearing zones, and the potential availability of groundwater for a community water supply. Laboratory analyses of samples from existing wells in the area was also carried out to determine the groundwater quality index (GWQI). Four vertical electrical sounding (VES) stations and nine profiles were surveyed using the Omega Campus and PQWT 150 instruments, respectively. The VES results delineated a maximum of five geo-electric sub-surface layers. A sudden change in the stratigraphy view of the rock formation from soft to very hard formation was observed in profile map L2. Profile map L7 and VES 2 has the highest potential for future groundwater exploration. Areas under VES 3 and profile maps L2, L3, L4, L5, L6, L8 and L9 are categorized as having a "medium" groundwater potential while the low yield water potential are areas under VES 1 and 4 and, profiles maps L1 and L10. The majority of groundwater in the weathered/fractured aquifer of the study area is slightly acidic. The GWQI values were less than 100, an indication that the analysed water samples fall within the "excellent" and "good" quality categories, implying that the groundwater is fit for domestic purposes. A combination of geophysical and physicochemical techniques has been successfully used to provide useful information for the assessment of groundwater potential and quality of the community.
机译:涉及地球物理和物理化学方法的综合方法是对地下水的潜在可用性及其质量在阿基·阿卡尤德塔尼日利亚省开展。电阻率和天然电场方法的组合用于描绘亚表面岩性,确定潜在的地下水区,以及地下水进行社区供水的潜在可用性。还进行了该地区现有井的样品的实验室分析,以确定地下水质量指数(GWQI)。使用欧米茄校园和PQWT 150仪器进行调查四个垂直电气探测(VES)站和九种型材。 VES结果最多划定了五个地质电亚表面层。在型材图L2中观察到从软到非常硬形成的岩层的地层视图的突然变化。型材地图L7和VES 2具有未来地下水勘探的最高潜力。 VES 3和轮廓图L2,L3,L4,L5,L6,L8和L9下的区域被分类为具有“培养基”的地下水电位,而低屈服水电位是VES 1和4下的区域,并且谱图L1和L10 。研究区域的风化/碎片含水层中的大多数地下水是微生物的。 GWQI值小于100,指示分析的水样落在“优秀”和“良好”的质量类别内,这意味着地下水适合国内目的。地球物理和物理化学技术的组合已成功地用于提供评估地下水潜力和社区质量的有用信息。

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