首页> 外文会议>Geotechnical Special Publication no.144; Multidisciplinary Conference; 20050924-28; San Antonio,TX(US) >Residual Potential Mapping of Contaminant Transport Pathways in Karst Formations of Southern Texas
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Residual Potential Mapping of Contaminant Transport Pathways in Karst Formations of Southern Texas

机译:德克萨斯州南部岩溶地层中污染物迁移途径的残留势图

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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:在得克萨斯州圣安东尼奥市附近一个受TCE污染的地点,利用剩余电位测绘(RPM)和高分辨率电阻率(HRR)进行了一次地球物理勘测。 RPM是一种基于“ mise-a-la-masse技术”的方法,其中,地下目标使用深处的直流传输源和接收器放置在地面上的规则网格上进行成像。RPM方法记录电势变化产生二维平面图的电势变化,RPM对这些特性的横向变化敏感,使其成为绘制断裂带和地下孔隙的极佳工具。相反,HRR是直接目前的方法是严格沿着线性样条线在地表上进行的;创建了电学特性的二维轮廓;紧密间隔和平行的HRR轮廓允许对地下进行三维重构;位于地面以下60至150英尺之间的多个传输位置,将接收器放置在310英尺乘300英尺的规则网格内的表面上。相对于假定均质性的建模背景电势,RPM响应高低。在同一RPM网格上总共收集了16个平行的HRR轮廓,调查深度约为60英尺。HRR收集的电阻率显示出通常的图形,即在表面附近具有高值,并且随着深度而减小。对轮廓进行背景去除以增强细微特征。去除背景的HRR轮廓用于创建三维图,显示可能的相互连接的岩溶特征路径。

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