ISSN 1000-3665 CN 11-2202/P

    海水入侵导水通道电阻率数值建模与层析成像

    Resistivity numerical modeling and tomography of seawater intrusion pathways

    • 摘要: 海水入侵是滨海地下工程面临的重要潜在威胁,准确查明其导水通道对风险防控和危害阻断具有关键意义。传统依赖于观测井和地下水样本分析的评估方法存在空间离散、时间滞后、成本高昂等固有缺陷,需要发展非侵入性、时空连续的高效探测技术,实现对海水入侵通道的快速识别与圈定。电阻率层析成像技术对富水破碎带、断层等低阻构造响应明显,能够有效反映地下介质电性差异,有助于快速便利地探查识别潜在的海水入侵通道。为提升探测精度与反演可靠性,采用有限元-无限元耦合法实现直流电阻率法高精度数值模拟;在此基础上,通过共轭梯度法开展针对海水入侵探查的电阻率层析成像反演研究。层状电阻率模型验证结果表明,耦合法显著提高了数值模拟精度,最大相对误差由传统有限单元法的30.7%降低至耦合法的1.7%;数值算例与工程实例进一步表明,电阻率层析成像可有效圈定海水入侵导水通道形成的低阻结构,成像结果与实际水文地质数据吻合良好,揭示了海水入侵的空间分布特征。电阻率层析成像可以实现快速面积性海水入侵相关水文调查工作,克服传统点状采样方法的局限性,可为滨海地下工程的前期选址勘察与后期监测维护等提供经济便利的勘探方法和技术支持,具有重要的工程应用价值。

       

      Abstract: Seawater intrusion poses a significant potential threat to coastal underground engineering, and the accurate identification of its preferential flow pathways is crucial for risk prevention and hazard mitigation. Traditional assessment methods relying on observation wells and groundwater sample analysis have inherent limitations, such as discrete spatial distribution, temporal lag, and high costs. Therefore, it is necessary to develop non-invasive, spatially, and temporally continuous efficient detection techniques to enable rapid identification and delineation of seawater intrusion pathways. Electrical resistivity tomography (ERT) presents a clear response to low-resistivity structures such as water-bearing fracture zones and faults, effectively reflecting the electrical property differences of subsurface media, and thus facilitates the rapid and convenient detection of potential seawater intrusion pathways. To improve detection accuracy and inversion reliability, a finite-infinite element coupling method was employed to achieve high-precision numerical simulation of the direct current resistivity method. On this basis, an ERT inversion study for seawater intrusion detection was conducted using the conjugate gradient method. Validation using a layered resistivity model shows that the coupled method significantly improves numerical simulation accuracy, reducing the maximum relative error from 30.7% with the traditional finite element method to 1.7% with the coupled method. Numerical examples and a field case further demonstrate that ERT can effectively delineate low-resistivity structures formed by seawater intrusion pathways, with imaging results showing good agreement with actual hydrogeological data and revealing the spatial distribution characteristics of seawater intrusion. ERT enables rapid and areal hydrogeological investigations related to seawater intrusion, overcoming the limitations of traditional point-based sampling methods. It provides an economical and convenient geophysical exploration approach and technical support for preliminary site selection surveys as well as subsequent monitoring and maintenance of coastal underground engineering, holding significant engineering application value.

       

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