• ISSN 2097-1893
  • CN 10-1855/P

DNAPLs 激发极化响应的室内实验与模拟研究

Laboratory experiment and simulation study on induced polarization response of DNAPLs

  • 摘要: 重非水相液体(dense non-aqueous phase liquids, DNAPLs)具有低溶解度、强挥发性和高致毒性等特点,修复难度较大. 精确掌握 DNAPLs 的污染范围是合理设计修复方案的前提. 非侵入式的激发极化法在污染场地表征方面有着很大的应用潜力. 然而,目前对于DNAPLs的激发极化信号变化影响因素较多,通过实验室测量获取电信号通常耗时耗力,且数据测量噪声大,难以对污染范围进行精细刻画和表征. 本研究通过砂柱批实验对DNAPLs污染土壤的电信号响应规律进行系统梳理,并提出一种基于数值模拟的DNAPLs污染砂柱的电信号响应分析方法. 实验结果显示电解液电导率和水饱和度均与相位负相关,与电导率正相关. 电解液电导率升高,引起孔隙水电导率的增加,双电层厚度被压缩,离子迁移率下降,极化强度降低. 随着水饱和度的增加,相位值降低,电导率值增加. 由于多孔介质内孔隙水的连通性增强,导电性增强,离子的迁移路径连续,电荷极化受阻,极化强度降低. 相位值和电导率值都随着粉土含量的增加而升高,因为通过阳离子交换增强了表面电导率和极化效应. 依托COMSOL Multiphysics与MATLAB平台,提出非饱和状态下的多孔介质复电导率模型,系统开展孔隙网络复电导率模拟,以验证和扩展实验结果. 提出的复电导率模型实现了电信号的数值模拟,在不同电解液电导率、水饱和度和土壤类型下的模拟结果与实验结果趋势一致,并改进了砂柱测量噪声大、耗时长的缺点,计算的结果呈现更好的数据可对比性. 本研究通过实验室测量与数值仿真相结合的方法,针对DNAPLs污染问题开展多维度研究. 研究结果不仅为DNAPLs在多孔介质中的赋存形态、迁移路径及其空间分布特征的精细化刻画提供了理论与方法支撑,更对构建基于非侵入式技术的DNAPLs污染场地识别-监测-修复一体化技术体系具有重要的科学价值与工程实践指导意义.

     

    Abstract: Dense non-aqueous phase liquids (DNAPLs) have characteristics such as low solubility, high volatility, and high toxicity, making their remediation particularly challenging. Accurately determining the extent of DNAPLs contamination is a prerequisite for designing an effective remediation plan. The non-invasive induced polarization (IP) method has great potential for application in site characterization of contaminated areas. However, there are many factors affecting the changes in the induced polarization signals of DNAPLs, and obtaining electrical signals through laboratory measurements is often time-consuming, labor-intensive, and subject to significant noise, making it challenging to precisely delineate and characterize the contaminated areas. This study systematically investigates the electrical signal response patterns of DNAPLs-contaminated soils through controlled laboratory batch experiments, and proposes a numerical simulation approach to study the electrical signal response of DNAPLs-contaminated sand columns. The results show that electrolyte conductivity and water saturation both have a negative correlation with phase, while showing a positive correlation with conductivity. This is because an increase in electrolyte conductivity directly leads to an increase in pore water conductivity, which compresses the thickness of the electrical double layer, decreases ion mobility, and reduces polarization intensity. The increase in water saturation enhances the connectivity of pore water in the porous medium, improving conductivity and providing a continuous path for ion migration, thus hindering charge polarization. Both phase and conductivity values increase with the increase in silt content, where cation exchange enhances surface conductivity and polarization effects. Based on COMSOL Multiphysics and MATLAB platforms, a complex conductivity model for unsaturated porous media is proposed, and a series of pore network complex conductivity simulations are conducted to verify and extend the experimental results. The proposed complex conductivity model enables the acquisition of electrical signals from a numerical simulation perspective, and the simulation results under different electrolyte concentrations, water saturations, and soil types are generally consistent with experimental trends. It also addresses the drawbacks of laboratory measurements, such as high noise and long measurement times, and the computed results show better data comparability. This study conducts a multidimensional investigation into DNAPLs contamination through a combination of laboratory measurements and numerical simulations. The results not only provide theoretical and methodological support for the detailed characterization of DNAPLs' existence forms, migration pathways, and spatial distribution characteristics in porous media, but also have significant scientific value and practical engineering guidance for the development of an integrated technology system for DNAPLs contamination site identification, monitoring, and remediation based on non-invasive techniques.

     

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