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Cross-hole electrical imaging of a controlled saline tracer injection

机译:受控盐水示踪剂注入的跨孔电成像

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Electrical imaging of tracer tests can provide valuable information on the spatial variability of solute transport processes. This concept was investigated by cross-borehole electrical imaging of a controlled release in an experimental tank. A saline tracer (conductivity 8 X 10(3) ms/m volume 270 1) was injected into a tank facility (dimensions 10 X 10 X 3 m) consisting of alternating sand and clay layers. Injection was from 0.3 m below the surface, at a point where maximum interaction between tank structure and tracer transport was expected. Repeated imaging over a two-week period detected non-uniform tracer transport, partly caused by the sand/clay sequence. Tracer accumulation on two clay layers was observed and density-driven spill of tracer over a clay shelf was imaged. An additional unexpected flow pathway, probably caused by complications during array installation, was identified close to an electrode array. Pore water samples obtained following termination of electrical imaging generally supported the observed electrical response, although discrepancies arose when analysing the response of individual pixels. The pixels that make up the electrical images were interpreted as a large number of breakthrough curves. The shape of the pixel breakthrough-recession curve allowed some quantitative interpretation of solute travel time, as well as a qualitative assessment of spatial variability in advective-dispersive transport characteristics across the image plane. Although surface conduction effects associated with the clay layers complicated interpretation, the plotting of pixel breakthroughs was considered a useful step in the hydrological interpretation of the tracer test. The spatial coverage provided by the high density of pixels is the factor that most encourages the approach. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 24]
机译:示踪剂测试的电子成像可以提供有关溶质传输过程的空间变异性的有价值的信息。通过跨孔电成像对实验储罐中的控制释放进行了研究。将盐水示踪剂(电导率8 X 10(3)ms / m体积270 1)注入由交替的沙子和粘土层组成的储罐设备(尺寸10 X 10 X 3 m)中。注入距离地面以下0.3 m,这是预计罐结构与示踪剂运输之间最大相互作用的点。经过两周的重复成像,发现示踪剂运输不均匀,部分是由沙子/粘土序列造成的。观察到示踪剂在两个黏土层上的堆积,并对示踪剂在黏土架子上溢出的密度驱动成像。在电极阵列附近发现了另一条意外流动路径,可能是由于阵列安装过程中的复杂性引起的。尽管在分析单个像素的响应时出现了差异,但是在电成像终止后获得的孔隙水样品通常支持观察到的电响应。构成电子图像的像素被解释为大量的突破曲线。像素突破-后退曲线的形状允许对溶质传播时间进行一些定量解释,并且可以对整个图像平面上的对流-弥散传输特征进行空间变异的定性评估。尽管与粘土层相关的表面传导效应使解释变得复杂,但像素突破的绘制被认为是示踪剂测试的水文解释中的有用步骤。高像素密度提供的空间覆盖范围是最鼓励采用该方法的因素。 (C)2000 Elsevier Science B.V.保留所有权利。 [参考:24]

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