胶州湾填海区三维电阻率模型构建与地质解译

Building and geological interpretation of a 3D resistivity model for the reclamation area of the Jiaozhou Bay

  • 摘要:
    背景 随着我国智慧城市化建设的深入推进,城市地下空间开发利用已成为热点,地球物理方法作为地下空间地质构造探测的重要技术手段,在应对城市复杂勘探环境时面临新挑战。
    目的和方法 针对青岛市滨海区域地下空间探测问题,选取胶州湾东岸围填海区作为研究区,采用圆锥型瞬变电磁与高密度电阻率联合探测技术,通过多源数据融合建立了三维电阻率模型,揭示了研究区地层结构和断裂破碎带范围,验证了圆锥型瞬变电磁法在复杂城市环境下的技术优势。
    结果和结论 研究区具有人工填土层−第四系沉积层−基岩三层电性结构特征,其中人工填土层底界面形态清晰;通过资料处理与地质解译,成功识别富水异常区及构造破碎带等不良地质体,分别表现为横向连续的电阻率变化带和等值线错断、下凹特征;由于基岩风化程度不同,断层和破碎带发育程度受到影响,在沧口断裂附近影响较大;建立的综合地球物理探测体系可以有效查明地层空间展布与构造发育特征,并为城市地下空间透明化提供了新的技术路径。研究成果可为地铁隧道选址、地下管网规划等工程应用提供重要地质依据。

     

    Abstract:
    Background With the advancement in smart city construction in China, the development and utilization of urban underground space have become a focal point. Geophysical methods, as a crucial technical means for underground geological structure exploration, face new challenges when applied to complex exploration environments in urban areas.
    Objectives and Methods  To address issues in underground space exploration in the coastal area of Qingdao, this study investigated the reclamation area along the eastern coast of the Jiaozhou Bay. Using a detection technique that combined the transient electromagnetic method (TEM) using a conical source and high-density resistivity method, this study constructed a 3D resistivity model through multi-source data fusion. This model revealed the stratigraphic structures and the extent of fracture zones within the study area, demonstrating the technical advantages of the novel TEM method with a conical source when applied to complex urban environments.
    Results and Conclusions  A three-layer electrical structure was revealed in the study area: an artificial fill layer, the Quaternary sedimentary layer, and bedrock. A clear bottom interface was observed in the artificial fill layer. Data processing and geological interpretation contributed to the successful identification of unfavorable geological bodies such as water-rich anomalous zones and structurally fractured zones, with the former exhibiting laterally continuous resistivity variation bands and the latter characterized by dislocated and concave contours. The varying degrees of bedrock weathering influenced the developmental degrees of faults and fracture zones, especially near the Cangkou fault. The established integrated geophysical exploration system can effectively identify the spatial distribution of strata and the characteristics of geological structures, providing a new technical pathway for achieving “transparent” urban underground space. The results of this study offer a critical geological basis for engineering applications such as metro tunnel siting and underground pipeline network planning.

     

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