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A comparison of self-potential tomography with electrical resistivity tomography for the detection of abandoned mineshafts

机译:自我电位层析成像与电阻率层析成像技术的比较,用于检测废弃的矿井

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摘要

We present a comparison of the abilities of Electrical Resistivity Tomography (ERT) and Self-Potential Tomography (SPT) to detect and characterize buried mineshafts at the site of a former colliery. Surface electrical resistivity and self-potential (SP) surveys were carried out at two test sites, each containing a hidden shaft. The ERT survey results indicate that both sites had a highly heterogeneous subsurface resistivity distribution, which we attribute to colliery spoil and former infrastructure. ERT managed to distinguish an air-filled, highly resistive mineshaft from this background, but failed to detect the second shaft, which was backfilled and therefore had a much lower resistivity contrast with the surrounding formation. However, SPT located both shafts, gave an indication of their size, shape and depth of burial, and was able to distinguish the open- from the backfilled mineshaft due to the strength of the associated SP anomalies. We argue that these SP anomalies are likely to be due to changes in the streaming potential caused by preferential drainage into the shafts. ud
机译:我们对电阻层析成像(ERT)和自电位层析成像(SPT)的能力进行比较,以检测和表征以前煤矿现场埋藏的矿井。在两个测试点进行了表面电阻率和自电位(SP)测量,每个测试点都包含一个隐藏的轴。 ERT调查结果表明,这两个地点的地下电阻率分布高度不均一,我们将其归因于煤矿破坏和以前的基础设施。 ERT设法从该背景中区分出充满空气的高电阻矿井,但未能检测到第二个井,该井被回填,因此与周围地层的电阻率对比低得多。但是,SPT定位了两个竖井,指示了它们的大小,形状和埋藏深度,并且由于相关SP异常的强度,能够区分开矿井和回填矿井。我们认为,这些SP异常很可能是由于优先排入井道而引起的流势变化所致。 ud

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