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Residual Potential Mapping of Contaminant Transport Pathways in Karst Formations of Southern Texas

机译:德克萨斯州南部喀斯特地层污染物运输途径的残余潜在映射

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An electrical geophysical survey, utilizing residual potential mapping (RPM) and high resolution resistivity (HRR), was completed at a TCE contaminated site near San Antonio, TX. RPM is a method based on the "mise-a-la-masse technique, where the subsurface target is imaged using a direct-current transmission source placed at depth, arid receivers placed on a regular grid on the surface. The RPM method records the disturbance in the potential field creating a two-dimensional plan view image of the changes in electrical properties. RPM is sensitive to lateral variations in these properties, making it an excellent tool for mapping facture zones and subsurface voids. Conversely, HRR is a direct-current method conducted strictly on the surface along linear transects. A two-dimensional profile of electrical properties is created. Closely spaced and parallel HRR profiles allow a three-dimensional reconstruction of the subsurface. Several transmitting locations, located between 60 and 150ft below ground surface, were used for the RPM survey. Receivers were placed on the surface within a regularized grid of 310ft by 300ft. The results of the RPM survey showed distinct areas of high and low RPM response, relative to a modeled background potential that assumes homogeneity. A total of 16 parallel HRR profiles were collected over the same RPM grid with a depth of investigation of approximately 60 ft. The electrical resistivity collected with HRR showed a general pattern of high values near the surface and decreasing values with depth. Background removal was conducted on the profiles to enhance subtle features. The background-removed HRR profiles were used to create a three-dimensional plot showing possible interconnected pathways of karst features.
机译:利用残留潜在的映射(RPM)和高分辨率电阻率(HRR)的电气地球物理调查在TCS污染的地点在San Antonio,TX附近完成。 RPM是一种基于“MISE-A-LA-Masse技术的方法,其中使用位于深度的直流传输源对地面上的地下目标进行了成像,干燥接收器放置在表面上的常规网格上。RPM方法记录潜在场中的干扰创建了电气变化的二维平面图图像。RPM对这些属性的横向变化敏感,使其成为映射实体区域和地下空隙的优秀工具。相反,HRR是直接的沿线横切严格地在表面上进行的电流方法。创建电气的二维轮廓。紧密间隔和平行的HRR配置文件允许地下的三维重建。几个透射位置,位于地面下方60到150英尺之间,用于转署调查。将接收器放在310英尺310英尺的正则电网内。RPM调查的结果表明截然不同相对于假设均匀性的建模的背景电位,高速和低的RPM响应。在相同的RPM网格上收集总共16个并行HRR型材,其进行大约60英尺的深度。用HRR收集的电阻率显示了表面附近的高值的一般图案,并用深度降低值。背景技术在曲线上进行以增强微妙的特征。背景删除的HRR配置文件用于创建三维图,显示岩溶特征的可能互连的互联路径。

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