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地球物理方法在城市地质结构精细化探测中最优方法组合研究——以成都市天府新区为例

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李华, 王东辉, 张伟, 杨剑, 王桥, 廖国忠, 王春山, 韩浩东, 席振铢, 王亮, 刘胜, 夏友刚, 李颖, 杨涛. 2023. 地球物理方法在城市地质结构精细化探测中最优方法组合研究——以成都市天府新区为例[J]. 中国地质, 50(6): 1691-1704. doi: 10.12029/gc20200509003
引用本文: 李华, 王东辉, 张伟, 杨剑, 王桥, 廖国忠, 王春山, 韩浩东, 席振铢, 王亮, 刘胜, 夏友刚, 李颖, 杨涛. 2023. 地球物理方法在城市地质结构精细化探测中最优方法组合研究——以成都市天府新区为例[J]. 中国地质, 50(6): 1691-1704. doi: 10.12029/gc20200509003
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LI Hua, WANG Donghui, ZHANG Wei, YANG Jian, WANG Qiao, LIAO Guozhong, WANG Chunshan, HAN Haodong, XI Zhenzhu, WANG Liang, LIU Sheng, XIA Yougang, LI Ying, YANG Tao. 2023. The application effect of geophysical method in fine exploration of urban geological structure and study of optimal combination method: A case study of Tianfu New Area in Chengdu, Sichuan Province[J]. Geology in China, 50(6): 1691-1704. doi: 10.12029/gc20200509003
Citation: LI Hua, WANG Donghui, ZHANG Wei, YANG Jian, WANG Qiao, LIAO Guozhong, WANG Chunshan, HAN Haodong, XI Zhenzhu, WANG Liang, LIU Sheng, XIA Yougang, LI Ying, YANG Tao. 2023. The application effect of geophysical method in fine exploration of urban geological structure and study of optimal combination method: A case study of Tianfu New Area in Chengdu, Sichuan Province[J]. Geology in China, 50(6): 1691-1704. doi: 10.12029/gc20200509003
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地球物理方法在城市地质结构精细化探测中最优方法组合研究——以成都市天府新区为例

  • 1.

    中国地质调查局成都地质调查中心, 四川 成都 610081

  • 2.

    中南大学地球科学与信息物理学院, 湖南 长沙 410083

  • 3.

    湖南五维地质科技有限公司, 湖南 长沙 410205

  • 4.

    中石化石油工程地球物理公司南方分公司, 四川 成都 610000

  • 5.

    四川华地建设工程有限责任公司, 四川 成都 610081

  • 基金项目:
    中国地质调查局项目（DD20189210、DD20190033）和国家自然科学青年基金（41804144）联合资助
详细信息
    作者简介: 李华, 男, 1979年生, 高级工程师, 主要从事工程地质、环境地质方面的地球物理勘查技术应用与研究; E-mail: 23841719@qq.com

  • 中图分类号: P631

The application effect of geophysical method in fine exploration of urban geological structure and study of optimal combination method: A case study of Tianfu New Area in Chengdu, Sichuan Province

  • 1.

    Chengdu Center, China Geological Survey, Chengdu 610081, Sichuan, China

  • 2.

    School of Geosciences and Info-physics, Central South University, Changsha 410083, Hunan, China

  • 3.

    Hunan 5D Geophyson Co., Ltd, Changsha 410205, Hunan, China

  • 4.

    SINOPEC Geophysical Corporation, Nanfang Branch, Chengdu 610041, Sichuan, China

  • 5.

    Sichuan Huadi Building Engineering Co., Ltd, Chengdu 618000, Sichuan, China

  • Fund Project: Supported by the projects of China Geological Survey (No.DD20189210, No.DD20190033) and National Natural Science Foundation of China (No.41804144)
More Information
    Author Bio: LI Hua, male, born in 1979, senior engineer, mainly engaged in the application and research of geophysical exploration in engineering and environmental geology; E-mail: 23841719@qq.com .

    摘要
  • 研究目的

    成都市天府新区属于典型的西南红层地区，其地层结构呈泥岩、粉砂质泥岩、泥质粉砂岩、砂岩互层结构，不同岩性之间的物性差异相对较小，研究浅部地质结构探测方法，有利于实现城市三维精细地质模型的建立。

     研究方法

    本文在成都天府新区4个典型试验区，采用多种新的和传统的地球物理方法开展了地质结构精细探测试验。

     研究结果

    地质雷达、三分量频率共振具有较高的分辨率，其次是浅层地震勘探、高密度电阻率法、等值反磁通瞬变电磁法、微动勘探；地质雷达和等值反磁通瞬变电磁抗干扰能力最强，浅震、三分量共振、微动勘探受城市噪音干扰比较严重；采用地质雷达、三分量频率共振、高密度电阻率法、等值反磁通瞬变电磁法、浅层地震、微动勘探等方法进行组合探测，可以获得由浅至深不同深度范围内的地质结构分层。

     结论

    通过对比分析每种方法的探测深度、分辨率、抗干扰强度、施工效率和经济成本，形成了适应于成都市天府新区不同工况、不同探测深度的地质结构精细探测地球物理方法最优组合方案。

    This paper is the result of urban geological survey engineering.

     Objective

    Tianfu New Area (TNA) of Chengdu is characterized by a typical red stratigraphy in southwest China, including interbed sedimentary rocks of mudstone, silty mudstone, argillaceous siltstone and sandstone. The difference of physical property among the above rocks is minor. Clarifying the shallow geological structure by geophysical method is favor for constructing the fine three-dimensional geological model of TNA.

     Methods

    This paper attempts to image fine geological structure in 4 typical sites of TNA through a variety of new and traditional geophysical methods.

     Results

    Ground penetrating radar (GPR) and three component frequency resonance (TCFR) have higher imaging resolution than that of shallow seismic exploration (SSE), electrical resistivity tomography (ERT), opposing coils transient electromagnetic (OCTEM) and microtremor exploration (ME). Urban noise tends to affect field data quality in SSE, TCFR and ME, but not in GPR and OCTEM. Fine geological structure from shallow to deep depth can be obtained by method assembly for GPR, TCFR, ERT, OCTEM, SSE and ME.

     Conclusions

    Under comparing and analyzing the detection depth, resolution, anti-urban noise level, construction efficiency, and economic cost of the above methods, the optimal geophysical method assembly to detect fine geological structure with different construction conditions and exploration depths in TNA of Chengdu is summarized.
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  • 图 1  成都市地质简图及试验点位置分布图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  成都市天府新区主要地层岩性电阻率和横波速度特征

    Figure 2. 

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    图 3  试验点一综合探测成果及推断解释图

    Figure 3. 

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    图 4  试验点二现场工况

    Figure 4. 

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    图 5  试验点二综合探测成果及推断解释图

    Figure 5. 

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    图 6  试验点三现场工况

    Figure 6. 

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    图 7  试验点三综合探测成果及推断解释图

    Figure 7. 

    下载: 全尺寸图片 幻灯片

    图 8  试验点四综合探测成果及推断解释图

    Figure 8. 

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    表 1  成都市天府新区主要地层岩性物性参数

    Table 1.  Physical parameters of different lithology in Tianfu New Area of Chengdu City

    下载: 导出CSV

    表 2  城市地球物理探测技术探测深度和主要优缺点分析统计

    Table 2.  Statistics of detection depth and main advantages and disadvantages of urban geophysical exploration technology

    下载: 导出CSV

    表 3  成都市天府新区地质结构探测方法最优组合方案

    Table 3.  Optimal combination scheme of geological structure detection methods in Tianfu New Area of Chengdu City

    下载: 导出CSV
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收稿日期:  2020-05-09
修回日期:  2020-05-23
刊出日期:  2023-12-25

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