Geo-electrostratigraphic assessment of aquifer potential, protectivity, and pliable level of vulnerability within a coastal milieu

N. Udosen, A. Ekanem, N.J. George, Jewel Thomas
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Abstract

Geo-electro stratigraphic assessments of aquifer potentiality, protectivity, and pliable level of vulnerability within a coastal milieu were undertaken with geo-electrical technology. The vertical electrical soundings were undertaken at 20 locations and the 2D electrical resistivity tomography surveys were undertaken at five locations within the study area. Results obtained from these geo-electrical surveys coupled with hydro-geophysical investigations within the area indicated the presence of four geo-electric layers: motley topsoil, sandy clay, fine sand, and coarse sand. The geo-stratigraphic data assessed groundwater potentiality, protectivity, and vulnerability to contamination with measures of transverse resistance, hydraulic conductivity, transmissivity, hydraulic diffusivity, aquifer storativity, and longitudinal conductance. Geo-hydraulic characterization indicated mean aquifer resistivity of 554.6 Ωm, mean aquifer conductivity of 0.0004 S/m, mean longitudinal conductance of 0.67 Ω−1, mean transverse resistance of 5601.7 Ωm2, mean hydraulic conductivity of 3.5 m/day, mean transmissivity of 283 m2/day, mean storativity of 0.0002, and mean hydraulic diffusivity of 1 × 105 m2/day. The results indicated that the region's groundwater potential ranged from medium to high. Longitudinal conductance values indicated that the aquifer protective capacity ranged from moderate to poor. Geo-electrical technology was therefore found to be an effective methodology for delineating aquifer potentiality, protectivity, and vulnerability within the vulnerable coastal aquifer system.
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对沿海环境中含水层的潜力、保护性和脆弱程度进行地质电法评估
利用地质电学技术对沿海环境中含水层的潜力、保护性和脆弱程度进行了地质电学地层评估。在研究区域内的 20 个地点进行了垂直电测,在 5 个地点进行了二维电阻率层析测量。这些地质电学勘测和该地区的水文地球物理勘测结果表明,该地区存在四个地质电学层:杂色表土层、砂质粘土层、细砂层和粗砂层。地质地层数据通过横向阻力、水力传导性、渗透性、水力扩散性、含水层蓄水量和纵向传导性等指标,评估了地下水的潜力、保护性和易受污染性。地质水文特征显示,含水层平均电阻率为 554.6 Ωm,含水层平均电导率为 0.0004 S/m,平均纵向电导率为 0.67 Ω-1,平均横向电阻率为 5601.7 Ωm2,平均水导率为 3.5 米/天,平均透射率为 283 平方米/天,平均蓄水率为 0.0002,平均水力扩散率为 1 × 105 平方米/天。结果表明,该地区的地下水潜力从中等到高等不等。纵向电导值表明,含水层的保护能力从中等到较差不等。因此,地质电学技术被认为是在脆弱的沿海含水层系统中划定含水层潜力、保护能力和脆弱性的有效方法。
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