Integrated geophysical and geochemical characterization of hydrocarbon contaminated site in Erhoike-Kokori, Southern Nigeria

O. S. Marere, O. J. Airen
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Abstract

The effectiveness of geophysical and geochemical methods in delineating hydrocarbon contamination in a spill site is carried out around theErhoike flow station in Kokori, Ethiope East LGA, Delta State. Wenner array was used for the transverse in acquiring the data which spanned a transverse of 200m and 3D model resistivity images were obtained from the inversion and presented in horizontal depth slices. Well water samples were also taken for Total Petroleum Hydrocarbon (TPH) content while soil samples from the location were also taken for Porosity and coefficient of permeability. The result of the 3D horizontal depth slices in the location reveals that Erhoike is impacted with hydrocarbon plume to a depth of 31.7m. The concentration of TPHCs from the water analysis shows that the wells around the suspected zones are affected by hydrocarbon. The laboratory tests for porosity (Փ ) and coefficient of permeability (k) for  the soil samples are indicative of sand/silty sand which thus allows the flow of PHCs plume to the soil and groundwater in the study area. The results of the study have shown that the soil is permeable and porous which would allow the passage of the leaked and spilled PHCs through the soil to groundwater where the PHCs could mix, float and sink into groundwater. The 3D analysis revealed the presence of PHCs up to a depth of 33.7m but prominent at a depth of 10m which indicates the presence of PHCs in the wells. The hydrochemical analysis also proved the same results as that of the 3D which authenticated the reliability of the method used in the study. 
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尼日利亚南部 Erhoike-Kokori 受碳氢化合物污染场地的综合地球物理和地球化学特征描述
在三角洲州 Ethiope East LGA 的 Kokori 的 Erhoike 流动站周围,对地球物理和地球化学方法在划定泄漏点碳氢化合物污染方面的有效性进行了研究。在获取横跨 200 米的数据时使用了温纳阵列,通过反演获得了三维电阻率模型图像,并以水平深度切片的形式呈现。还采集了井水样本以检测总石油烃 (TPH) 含量,同时采集了该地点的土壤样本以检测孔隙度和渗透系数。该地点的三维水平深度切片结果显示,Erhoike 受碳氢化合物羽流影响的深度为 31.7 米。水分析得出的 TPHCs 浓度表明,疑似区域周围的水井受到了碳氢化合物的影响。土壤样本的孔隙度(Փ)和渗透系数(k)的实验室测试表明,土壤样本为砂质/粉砂质,因此允许 PHCs 羽流进入研究区域的土壤和地下水。研究结果表明,土壤具有渗透性和多孔性,这使得泄漏和溢出的 PHC 可以通过土壤进入地下水,在地下水中混合、漂浮并沉入地下水。三维分析表明,在 33.7 米深的地方存在 PHCs,但在 10 米深的地方比较突出,这表明水井中存在 PHCs。水化学分析也证明了与三维分析相同的结果,这证明了研究中所使用方法的可靠性。
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