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基于高密度电法的城市岩溶地下水通道三维电性成像

刘道涵 徐俊杰 齐信 邬健强

刘道涵,徐俊杰,齐 信,等. 基于高密度电法的城市岩溶地下水通道三维电性成像[J]. 中国岩溶,2023,42(6):1331-1338 doi: 10.11932/karst20230615
引用本文: 刘道涵,徐俊杰,齐 信,等. 基于高密度电法的城市岩溶地下水通道三维电性成像[J]. 中国岩溶,2023,42(6):1331-1338 doi: 10.11932/karst20230615
LIU Daohan, XU Junjie, QI Xin, WU Jianqiang. Three-dimensional electrical imaging of urban karst groundwater channels based on electrical resistivity tomography[J]. CARSOLOGICA SINICA, 2023, 42(6): 1331-1338. doi: 10.11932/karst20230615
Citation: LIU Daohan, XU Junjie, QI Xin, WU Jianqiang. Three-dimensional electrical imaging of urban karst groundwater channels based on electrical resistivity tomography[J]. CARSOLOGICA SINICA, 2023, 42(6): 1331-1338. doi: 10.11932/karst20230615

基于高密度电法的城市岩溶地下水通道三维电性成像

doi: 10.11932/karst20230615
详细信息
    作者简介:

    刘道涵(1987-),男,高级工程师,主要研究方向为地球物理方法及应用研究。E-mail:ldhwcgs@163.com

    通讯作者:

    邬健强(1990-),男,高级工程师,主要研究方向为地球物理方法及应用研究。E-mail:1191261549@qq.com

  • 中图分类号: P631.3

Three-dimensional electrical imaging of urban karst groundwater channels based on electrical resistivity tomography

  • 摘要: 岩溶地下水通道是隐伏岩溶区常见的地质现象,开展城市隐伏岩溶通道探测对城市地下空间开发和地质灾害防治具有重要意义。岩溶通道常具有高度的空间变异性,常规二维探测难以对其进行较好的表征。基于此,文章采用三维高密度电法对城市隐伏岩溶地下通道进行了精细探测,结合地球物理数值模拟和应用实例,分析三维高密度电法对不同充填类型岩溶地下通道的成像效果。结果表明:三维高密度电法较二维探测在数据量和分辨率上均有较大提升,可更直观地表征目标体三维电性结构特征,该探测方法对岩溶地下水通道成像具有优势;通过对武汉市源泉村岩溶地下水通道三维电性成像,揭示了该低温热泉的地下水运移特征,可为城市地热勘探开发提供参考。

     

  • 图  1  三维高密度电法模拟计算

    a:三维模型 b:正演视电阻率数据 c:三维反演结果切片 d: 反演电性异常体

    Figure  1.  Simulation calculation from 3D ERT

    a: 3D Model b: Forward modeling c: Slices inversed by 3D ERT d: The anomalous body inversed by 3D ERT

    图  2  地表泉点工作区示意图

    Figure  2.  Schematic diagram of work area in the surface spring

    图  3  地表泉点二维高密度电法探测结果

    Figure  3.  Results of 2D ERT in the surface spring

    图  4  地表泉点三维高密度电法反演结果

    (a:三维反演结果切片 b:圈定地下水流通道)

    Figure  4.  Results inversed by 3D ERT in the surface spring

    (a: Slices inversed by 3D ERT b: The boundary of groundwater channel)

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出版历程
  • 收稿日期:  2022-02-13
  • 网络出版日期:  2023-12-28
  • 刊出日期:  2023-12-01

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