ISSN 1000-3665 CN 11-2202/P

    基于高密度电法的堤坝含水率时空成像与渗漏监测

    Spatiotemporal imaging of water content and monitoring of seepage hazards in embankments using electrical resistivity tomography method

    • 摘要: 现有堤坝渗漏隐患探查方法中,钻探存在成本高、效率低、探测结果“一孔之见”等问题,物探方法常依赖于对地球物理参数解译进行间接探测,无法直观揭露渗漏隐患。为实现堤坝渗漏隐患的高效、直观表征与演化过程监测,以含水率为渗漏隐患直观表征参数,提出基于高密度电阻率法的含水率时空成像方法,并利用光纤及水文地质监测数据进行对比验证。以烟台方里水库作为研究区,分析土样、岩芯含水率与地电参数的相关关系并建立定量的含水率预测模型;提出基于混合Lp范数约束的电阻率反演方法,建立三维地电模型重构方法,融入时间约束实现监测数据较准确的反演;设计2条高密度电阻率测线,于汛期中、后开展监测,实现电阻率、含水率的时空成像。电阻率、含水率成像结果揭示了下游坝坡的浅层高含水率含砂壤土层及其三维分布特征,时移成像表明监测期间部分区域含水率有所升高,位移、水位、水温监测数据显示坝体结构尚未出现显著破坏迹象。高含水率异常可能源于壤土压实度不足、降水事件或潜在渗漏等,建议加强后续探测与监测。本研究实现了由传统电阻率到含水率三维分布及时移演化的时空成像,验证了基于含水率时空成像开展土石坝渗漏隐患探查监测的有效性。

       

      Abstract: Reliable detection and monitoring of seepage hazards in embankment dams remain challenging. Conventional approaches, such as drilling, are costly and provide only point-scale information, whereas geophysical methods often rely on indirect proxies that limit intuitive interpretation of seepage processes. To enable efficient and intuitive characterization of seepage hazards, this study proposed a spatiotemporal imaging approach for water content based on high-density electrical resistivity tomography (ERT). In the area of Fangli Reservoir in Yantai City, water content was selected as a direct indicator of seepage hazards. Correlations between water content and geoelectrical parameters of soil and rock-core samples were analyzed to establish a quantitative prediction model. A mixed Lp-norm-constrained inversion method, a 3D geoelectrical reconstruction workflow, and temporal constraints were further introduced to improve the inversion of monitoring data. Two high-density ERT lines were deployed on the downstream slope, and monitoring surveys were conducted during and after the flood season to obtain spatiotemporal images of resistivity and water content. Fiber-optic and hydrogeological monitoring data were used for validation. The imaging results reveal a shallow sandy loam layer with high water content on the downstream slope and delineate its three-dimensional distribution characteristics. Time-lapse imaging indicates that water content increases in some areas during the monitoring period. Displacement, water-level, and water-temperature data suggest no significant structural damage to the embankment. High-water-content anomalies may be associated with insufficient soil compaction, precipitation, and potential seepage. Early warning and strengthened follow-up investigation and monitoring are therefore recommended. The results demonstrate that water-content-based spatiotemporal imaging is effective for seepage hazard detection and monitoring in reservoir embankments.

       

    /

    返回文章
    返回