拉各斯Abule Ado IJEDODO地区油气泄漏地电层析成像研究

O. O. Adeoye-Oladapo, M. I. Oladapo
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引用次数: 1

摘要

为了确定拉各斯Abule Ado Ijedodo地区Ijedodo石油管道路线Ijedodo段碳氢化合物泄漏所造成的污染程度,进行了地质层析成像研究。现场研究采用了偶极-偶极电极结构的电阻率层析成像方法。导线长度为1870 m,电极间距为10 m,偶极间分离因子(n)在1 ~ 8之间变化。研究区下部为达荷美沉积盆地。数据呈现为沿二维电阻率结构的场和理论伪剖面。二维电阻率结构输出对现场数据进行了反演,以获得用于地下表征的模型。观察到的高电阻率值归因于电阻砂单元,而获得的低电阻率值是导电粘土单元的诊断。然而,记录到的异常高电阻率值是由于油气侵入了一些孔隙空间。偶极子-偶极子场和理论伪剖面显示,在研究段的南半部(1000 m)下方,导电(粘土)材料占主导地位,夹杂着轻微的电阻(砂)材料。在烃污染点下圈定了一个孤立的导电特征(粘土)。然而,有限差分反演剖面在180 ~ 970 m至约23 m深度范围内呈现出低电阻率物质(推测为粘土)构成的顶部段。该剖面在390 - 940米和1740 - 1870米附近的下部段呈现异常的高电阻率成分(诊断严重的碳氢化合物影响)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geoelectric Tomography Study of Hydrocarbon Spill at IJEDODO Area, Abule Ado, Lagos
Geo-tomography study has been undertaken to determine the level of pollution occasioned by hydrocarbon spill at Ijedodo section of petroleum pipeline route at Ijedodo area of Abule Ado, Lagos. The field study involved the electrical resistivity tomography method using Dipole-Dipole electrode configuration. Traverse length of 1,870 m was occupied with electrode separations of 10 m and inter-dipole separation factor (n) varied from 1 to 8. The study area is underlain by the Dahomey Sedimentary Basin. The data are presented as field and theoretical pseudosections alongside 2-D resistivity structure. 2-D Resistivity Structure output presents inversion of the field data to obtain a model utilized for subsurface characterization. Observed high resistivity values are attributable to resistive sand units while low values obtained are diagnostic of conductive clay units. However, anomalously high resistivity values recorded are attributable to hydrocarbon invasion of some pore spaces. Dipole-Dipole field and theoretical pseudosections generated for the segment show predominance of conductive (clay) materials interspersed with slightly resistive (sand) materials beneath the southern half (1000 m) of the investigated segment. An isolated conductive feature (clay) was delineated beneath hydrocarbon pollution point. Finite Difference Method (FDM) inversion section of the investigated section however presents low resistivity materials (presumably clay) constituting the top segment within 180 – 970 m to depth of about 23 m. The section presents anomalously high resistivity constituents (diagnostic of severe hydrocarbon impact) at the lower segment in areas around 390 – 940 m and 1740 – 1870 m.
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