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Electrical resistivity and induced polarization tomography in identifying the plume of chlorinated hydrocarbons in sedimentary formation: a case study in Rho (Milan - Italy)

机译:电阻率和感应极化层析成像技术在确定沉积物中含氯烃羽流的过程中:以罗镇为例(意大利米兰)

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摘要

Resistivity and induced polarization surveying were originally developed for mineral exploration but are now finding new applications in the field of environmental and engineering geophysics. The present article reports the results of a geophysical survey performed with the aim of identifying a plume of chlorinated hydrocarbons in sedimentary formations of the Pandania plain. The tested site is characterized by three sand and gravel aquifers containing a quantity of clay particles which influence the overall bulk resistivity and chargeability. According to data obtained using shallow boreholes, mainly dense non-aqueous phase liquids were found as contaminants in the first and second aquifer. The aforementioned geo-electrical methods were applied in both two- and three-dimensional approaches. Steel and copper electrodes were used in the process of field data acquisition and the results of the survey were compared. The geophysical survey revealed some anomalies that could be explained by the presence of dense non-aqueous phase liquids in the soil medium. The concept of normalized chargeability facilitates the interpretation of detected induced polarization anomalies. The shape of the plume was inferred from maps of resistivity and chargeability to a depth of 25 m below the surface of the ground.
机译:电阻率和感应极化勘测最初是为矿物勘探而开发的,但现在在环境和工程地球物理学领域中找到了新的应用。本文报告了一项地球物理调查的结果,旨在确定潘丹尼亚平原沉积岩层中的氯化烃羽流。测试地点的特征是三个砂砾石含水层,其中包含一定数量的粘土颗粒,这些粘土颗粒会影响整体体积电阻率和带电性。根据使用浅孔获得的数据,在第一和第二含水层中发现了主要是稠密的非水相液体作为污染物。前述的地电方法被应用于二维和三维方法中。在现场数据采集过程中使用了钢和铜电极,并比较了调查结果。地球物理调查揭示了一些异常现象,可以解释为土壤介质中存在稠密的非水相液体。归一化荷电率的概念有助于解释检测到的感应极化异常。烟羽的形状是根据电阻率和可充电性的图推断出来的,其深度为地面以下25 m。

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