ISSN 1000-3665 CN 11-2202/P

    地下水地球物理研究进展与前沿展望

    Groundwater geophysics: Progress and prospects

    • 摘要: 地下水地球物理是水文地质学与地球物理学交叉形成的重要学科方向,在地下水系统结构识别、水文参数反演及动态过程监测中发挥着关键作用。本次概述了该领域的主要探测方法、典型应用进展及前沿发展方向。电阻率法、地震法、电磁法、探地雷达及核磁共振等技术各具适用尺度与灵敏度,多方法联合监测与岩石物理建模是实现定量解释的核心。围绕典型应用场景,研究包括:多相流机理与污染场地刻画揭示了孔隙中非水相污染的地球物理响应规律,并发展了场地尺度的实时监测与动态采样调查体系;岩溶与裂隙水探测展示了多源信息约束反演与时移电阻率技术在复杂覆盖层下的高分辨率成像能力;海水入侵与堤坝渗漏监测突出了高精度正演模拟与含水率时空成像在工程隐患识别中的应用;地震与地下水相互作用从多场耦合角度阐释了流体与地震活动的互馈机制。当前面临高分辨率探测、岩石物理模型适用性、四维反演稳定性及多源数据融合等挑战,未来应重点发展高精度探测装备、岩石物理定量模型、时移监测技术、联合反演框架及人工智能融合方法。

       

      Abstract: Groundwater geophysics is an important interdisciplinary field at the intersection of hydrogeology and geophysics, playing a pivotal role in groundwater system structure identification, hydrological parameter inversion, and dynamic process monitoring. Based on this special issue, this article outline the primary detection methods, typical application advancements, and frontier development directions in groundwater geophysics. Methods such as electrical resistivity, seismic, electromagnetic, ground-penetrating radar, and nuclear magnetic resonance, each possess unique applicable scales and sensitivities, with multi-method monitoring and petrophysics modeling serving as the core for quantitative interpretation. Based on typical application scenarios, this mini review includes: multiphase flow mechanisms and contaminated site characterization, which reveal the geophysical response patterns of non-aqueous phase contaminants in pores and have developed real-time monitoring and dynamic sampling investigation systems at the site scale; karst and fractured water detection, demonstrating the high-resolution imaging capabilities of multi-source information-constrained inversion and time-lapse resistivity techniques under complex cover layers environment; seawater intrusion and dam leakage monitoring, highlighting the application of high-precision forward modeling and moisture content spatiotemporal imaging in identifying engineering hazards; and seismic-groundwater interaction, elucidating the feedback mechanisms between fluids and seismic activity from a multi-field coupling perspective. Current challenges include high-resolution detection, petrophysics model applicability, 4D inversion stability, and multi-source data integration. Future efforts should prioritize the development of high-resolution detection equipment, quantitative petrophysics models, time-lapse monitoring technologies, joint inversion frameworks, and AI-integrated methodologies.

       

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