Enhanced contamination risk assessment for aquifer management using the geo-resistivity and DRASTIC model in alluvial settings

N.J. George , O.E. Agbasi , A.J. Umoh , A.M. Ekanem , N.I. Udosen , J.E. Thomas , M.U. Aka , J.S. Ejepu
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Abstract

This study employs geo-electric surveys and Vertical Electrical Sounding (VES) data, as well as a spatiotemporal assessment, to evaluate aquifer characteristics in the study area, with the main thrust of revealing significant subsurface variability, vulnerability, and the consequent contamination of an aquifer system already established to be prolific. The study employed the DRASTIC model, integrated with geophysical resistivity methods, to assess groundwater vulnerability. Using Schlumberger electrode configurations, resistivity surveys at 19 VES locations provided insights into key aquifer parameters, including depth to groundwater, aquifer media, and vadose zone impact. This approach enhanced parameter accuracy for robust vulnerability assessments.The aquifers, primarily composed of fine to gravelly sands from the Benin Formation, exhibit high porosity and permeability. However, discrepancies in transmissivity, hydraulic conductivity, and permeability point to inconsistent groundwater behavior. Groundwater vulnerability, evaluated using the DRASTIC Index (DI), is classified as moderate to high, with influencing factors such as shallow water table depth (28 %), vadose zone properties (25 %), and net recharge (20 %). Predominantly H and K curve types suggest moderate to high contamination risks, while the region's topography and arenitic lithology exacerbate vulnerability due to slower filtration rates. The study emphasizes the need for careful groundwater management, given the aquifer's susceptibility to contamination. Regular monitoring is recommended, particularly in densely populated or agriculturally active areas, to mitigate contamination risks associated with the area's high permeability, porosity, and recharge variability. The DRASTIC model improves contamination risk assessment in sedimentary environments by analyzing several factors: depth to water (DTW), net recharge (NR), aquifer media (AM), soil media (SM), topography (T), the vadose zone (IPVZ), and hydraulic conductivity (C). Among these, DTW, IPVZ, and NR were the most sensitive contributors to the DRASTIC index (DI) for assessing vulnerability. AM and SM were moderately sensitive, while T and C had minimal impact. To effectively mitigate contamination, priority should be given to DTW, AM, and SM, with less focus on T and C. These insights help in better resource allocation and sustainable aquifer management.
利用地质电阻率和DRASTIC模型在冲积层管理中加强污染风险评估
本研究采用地电测量和垂直电测深(VES)数据以及时空评估来评估研究区域的含水层特征,其主要目的是揭示已经建立的丰富含水层系统的显著地下变异性、脆弱性以及随之而来的污染。采用DRASTIC模型,结合地球物理电阻率法对地下水脆弱性进行评价。使用斯伦贝谢的电极配置,在19个VES位置进行电阻率调查,可以深入了解关键的含水层参数,包括地下水深度、含水层介质和渗透层的影响。该方法提高了鲁棒性脆弱性评估参数的准确性。该含水层主要由贝宁组的细砂至砾石砂组成,具有较高的孔隙度和渗透率。然而,透过率、水力导电性和渗透率的差异表明地下水的行为不一致。利用DRASTIC指数(DI)评价的地下水脆弱性分为中至高,影响因素包括浅层地下水位深度(28 %)、渗透带性质(25 %)和净补给(20 %)。主要的H和K曲线类型表明中度至高度污染风险,而该地区的地形和砂质岩性由于过滤速度较慢而加剧了脆弱性。该研究强调,考虑到含水层易受污染,需要谨慎地管理地下水。建议定期监测,特别是在人口稠密或农业活跃的地区,以减轻与该地区高渗透率、孔隙度和补给可变性相关的污染风险。DRASTIC模型通过分析水深(DTW)、净补给(NR)、含水层介质(AM)、土壤介质(SM)、地形(T)、渗透带(IPVZ)和导水率(C)等因素,改进了沉积环境污染风险评价。其中,DTW、IPVZ和NR对DRASTIC指数(DI)的影响最为敏感。AM和SM中度敏感,而T和C影响最小。为了有效减轻污染,应优先考虑DTW、AM和SM,而不是T和c。这些见解有助于更好地分配资源和可持续的含水层管理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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