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炭质灰岩地区抽水致塌控制因素和影响因素

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文章导航 > 中国地质灾害与防治学报 > 2021 > 32(4): 65-72

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唐灵明, 陈学军, 黄翔, 毕鹏雁, 张晓宸. 炭质灰岩地区抽水致塌控制因素和影响因素——以广西兴安县为例[J]. 中国地质灾害与防治学报, 2021, 32(4): 65-72. doi: 10.16031/j.cnki.issn.1003-8035.2021.04-09
引用本文: 唐灵明, 陈学军, 黄翔, 毕鹏雁, 张晓宸. 炭质灰岩地区抽水致塌控制因素和影响因素——以广西兴安县为例[J]. 中国地质灾害与防治学报, 2021, 32(4): 65-72. doi: 10.16031/j.cnki.issn.1003-8035.2021.04-09
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TANG Lingming, CHEN Xuejun, HUANG Xiang, BI Pengyan, ZHANG Xiaochen. Controlling and influencing factors of the karst collapse caused by withdrawing of groundwater in carbonaceous limestone area:A case study of Xing'an County, Guangxi Province[J]. The Chinese Journal of Geological Hazard and Control, 2021, 32(4): 65-72. doi: 10.16031/j.cnki.issn.1003-8035.2021.04-09
Citation: TANG Lingming, CHEN Xuejun, HUANG Xiang, BI Pengyan, ZHANG Xiaochen. Controlling and influencing factors of the karst collapse caused by withdrawing of groundwater in carbonaceous limestone area:A case study of Xing'an County, Guangxi Province[J]. The Chinese Journal of Geological Hazard and Control, 2021, 32(4): 65-72. doi: 10.16031/j.cnki.issn.1003-8035.2021.04-09
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炭质灰岩地区抽水致塌控制因素和影响因素

  • 1.

    桂林理工大学土木与建筑工程学院，广西 桂林　541004

  • 2.

    广西岩土力学与工程重点实验室，广西 桂林　541004

  • 3.

    广西岩溶动力学重点实验室，广西 桂林　541004

  • 基金项目: 国家自然科学基金（41967037）；广西岩溶动力学重点实验室开放课题基金(YR-JJHT-2016-466)
详细信息
    作者简介: 唐灵明（1987-），男，广西桂林人，地质资源与地质工程专业，硕士研究生，工程师，主要从事岩土工程、地质灾害预测与防治研究。E-mail：262611613@qq.com
    通讯作者: 陈学军（1961-），男，广西桂林人，地质工程专业，博士研究生，教授，主要从事岩土工程、灾害地质与环境工程方面的教学和研究工作。E-mail: chenxj@glut.edu.cn

  • 中图分类号: P642.26

Controlling and influencing factors of the karst collapse caused by withdrawing of groundwater in carbonaceous limestone area:A case study of Xing'an County, Guangxi Province

  • 1.

    College of Civil and Architectural Engineering, Guilin University of Technology, Guilin, Guangxi　541004, China

  • 2.

    Guangxi Key Laboratory of Geomechanics and Geotechnical Engineering, Guilin, Guangxi　541004, China

  • 3.

    Open Research Fund of Guangxi Karst Dynamics Laboratory, Guilin, Guangxi　541004, China

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    摘要

  • 为研究炭质灰岩地区抽水致塌控制因素和影响因素，通过电法物探、地质钻探及抽水致塌试验相结合的综合手段，对兴安县石炭系下统岩关组（C1y）炭质灰岩地区的岩溶塌陷进行关联分析，建立降深水位与时间、恢复水位与时间的关系对比曲线。研究结果表明：在炭质灰岩地区进行抽水活动时，其主要补给源为小溶洞内储存水，运输通道为岩溶裂隙；该炭质灰岩地区岩溶裂隙具有不规则性，因此，在同类地层中测得的渗透系数k及影响半径R有较大差异；研究区域内抽水致塌的位置受地质构造的影响较为明显；钻井人为抽水致塌受多种因素共同作用影响，而地下水位升降为主要影响因素。

    For the study of the model of pumping collapse in carbonaceous limestone area, through the combination of electrical geophysical prospecting, geological drilling and pumping collapse test, this paper conducted the correlation analysis of karst collapse in carbonaceous limestone area of Lower Carboniferous Yanguan formation (C1y) in Xing’an County, and established the correlation curves between drawdown water level and time and recovery water level and time. The results denotes that: The main supply source is water stored in small karst caves and the transfer passage are cave and karst fissures when pumping in calcareous limestone area. The karst fissures in the calcareous limestone area are irregular, so the permeability coefficient and influence radius measured in similar strata are quite different. The location of collapse caused by pumping in the study area is obviously affected by geological structure. When pumping produces excessive drawdown, the karst collapse often occurs at the fracture zone of aquifer. The collapse caused by man-made pumping is affected by many factors, and the rise and fall of groundwater level is the main factor.

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  • 图 1  钻井结构图

    Figure 1. 

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    图 2  同一钻井三次定流量抽水试验曲线对比

    Figure 2. 

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    图 3  同一钻井三次定流量水位恢复试验曲线对比

    Figure 3. 

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    图 4  研究区电法工作布置平面图

    Figure 4. 

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    图 5  研究区联合剖面ρs剖面平面图

    Figure 5. 

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    图 6  研究区2线不同供电极距联剖对比曲线

    Figure 6. 

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    图 7  研究区2线视电阻率(${\boldsymbol{\rho }}_{\rm{s}}$)断面等值线图

    Figure 7. 

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收稿日期:  2020-07-25
修回日期:  2021-01-15
刊出日期:  2021-08-25

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