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Site suitability for engineering‑infrastructure (EI) development and groundwater exploitation using integrated geophysical approach in Guangdong, China

机译:工程 - 基础设施(EI)开发和地下水利用中国广东综合地球物理方法的现场适用性

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摘要

This study describes the efficiency of an incorporated geophysical approach involving ERT (electrical resistivity tomography), magnetic, induced polarization (IP), and self-potential (SP), with a view to investigate subsurface of a highly heterogeneous site for EI (engineering infrastructure) development and groundwater exploitation in Huidong County, Guangdong, China. The subsurface formation can be delineated using boreholes; however, such approaches are time consuming, expensive, and cannot be carried out in the steep topographic areas. The proposed geophysical approach can decrease significant number of boreholes to evaluate the most problematic geologic structures. The geophysical data were acquired via a variety of survey parameters along four profiles. A least-squares inversion technique was used for the post-processing of geophysical data to generate 2D/3D models of the subsurface geologic units. ERT/magnetic results combined with borehole data delineated four distinct layers with specific resistivity range, such as the topsoil cover, the highly weathered layer, the semi-weathered layer, and the fresh bedrock. Incorporation of ERT/magnetic models with IP and SP delineated several localized fractures/faults. Empirical equations were obtained to estimate hydraulic conductivity of the weathered layer. The integrated results propose that groundwater is the best accessible in weathered/fractured zones, whereas such zones are unsuitable for the construction of engineering infrastructures. The geophysical results show high correlation with accessible upfront borehole information of the investigated site. The study suggests that this integrated approach can be used as a useful tool in any heterogeneous site for suitability of EI development and groundwater exploitation.
机译:本研究描述了涉及ert(电阻率断层扫描),磁,诱导极化(IP)和自我电位(SP)的掺入的地球物理方法的效率,以研究EI高度异构位点的地下(工程基础设施中国广东省惠东县的开发和地下水开采。地下地层可以使用钻孔描绘;然而,这种方法是耗时,昂贵的,并且不能在陡峭的地形区域中进行。所提出的地球物理方法可以降低大量的钻孔以评估最有问题的地质结构。通过四个简档通过各种调查参数获取地球物理数据。最小二乘反转技术用于地球物理数据的后处理,以产生地下地质单元的2D / 3D模型。 ERT /磁性效果与钻孔数据相结合,描绘了具有特定电阻率范围的四个不同的层,如表土盖,高度风化层,半风化层和新的基岩。使用IP和SP掺入ERT /磁模型划定了几种局部裂缝/故障。获得经验方程以估计风化层的液压导电性。综合结果提出了地下水是风化/骨折区域最佳的可接近,而这种区域不适合建造工程基础设施。地球物理结果表明,与调查部位的可接近的前孔信息显示出高的相关性。该研究表明,这种综合方法可以用作任何异构位点的有用工具,以适合EI开发和地下水开采。

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  • 作者单位

    Chinese Acad Sci Inst Geol & Geophys Key Lab Shale Gas & Geoengn 19 Beitucheng Western Rd Beijing 100029 Peoples R China|Chinese Acad Sci Innovat Acad Earth Sci Beijing 100029 Peoples R China|Univ Chinese Acad Sci Coll Earth & Planetary Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Geol & Geophys Key Lab Shale Gas & Geoengn 19 Beitucheng Western Rd Beijing 100029 Peoples R China|Chinese Acad Sci Innovat Acad Earth Sci Beijing 100029 Peoples R China|Univ Chinese Acad Sci Coll Earth & Planetary Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Geol & Geophys Key Lab Shale Gas & Geoengn 19 Beitucheng Western Rd Beijing 100029 Peoples R China|Chinese Acad Sci Innovat Acad Earth Sci Beijing 100029 Peoples R China|Univ Chinese Acad Sci Coll Earth & Planetary Sci Beijing 100049 Peoples R China;

    CAS HEC China Pakistan Joint Res Ctr Earth Sci Islamabad 45320 Pakistan|Quaid i Azam Univ Dept Earth Sci Islamabad 45320 Pakistan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Resistivity; Magnetics; Inversion; Engineering infrastructures; Groundwater; Hydraulic conductivity;

    机译:电阻率;磁性;反演;工程基础设施;地下水;液压导电性;

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