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井-孔联合疏排高填方滑坡地下水典型案例分析

赖国泉, 焦海平

赖国泉,焦海平. 井-孔联合疏排高填方滑坡地下水典型案例分析[J]. 中国地质灾害与防治学报,2024,35(4): 106-114. DOI: 10.16031/j.cnki.issn.1003-8035.202306020
引用本文: 赖国泉,焦海平. 井-孔联合疏排高填方滑坡地下水典型案例分析[J]. 中国地质灾害与防治学报,2024,35(4): 106-114. DOI: 10.16031/j.cnki.issn.1003-8035.202306020
LAI Guoquan,JIAO Haiping. Analysis of typical cases of groundwater in high fill landslide with combined well-hole drainage[J]. The Chinese Journal of Geological Hazard and Control,2024,35(4): 106-114. DOI: 10.16031/j.cnki.issn.1003-8035.202306020
Citation: LAI Guoquan,JIAO Haiping. Analysis of typical cases of groundwater in high fill landslide with combined well-hole drainage[J]. The Chinese Journal of Geological Hazard and Control,2024,35(4): 106-114. DOI: 10.16031/j.cnki.issn.1003-8035.202306020

井-孔联合疏排高填方滑坡地下水典型案例分析

基金项目: 中国中铁股份有限公司科技研究开发计划(2022-重大专项-07);中铁九局科技开发计划(YGSJSZX202308-01)
详细信息
    作者简介:

    赖国泉(1981—),男,硕士,高级工程师,主要从事岩土工程研究工作。E-mail:273085646@qq.com

  • 中图分类号: P642.22

Analysis of typical cases of groundwater in high fill landslide with combined well-hole drainage

  • 摘要:

    以攀枝花机场13#滑坡治理工程为例,在简述滑坡基本概况的基础上,着重论述了研究区水文地质条件。研究区雨季降水量占全年降水量的95%,中−大暴雨、3 d及以上降雨天数出现次数集中于7—9月,占总数的95%以上。研究区降雨具有雨季降水量强度大且集中的特点。物探及钻探揭示,滑坡后缘场坪填方区地下水丰富,具有“窝”状不连续分布特征,有明显的成层性;含水层具有黏土含量高、赋水性较好、孔隙连通性差、径流不畅,坡内地下水难以快速消散等特点。基于该滑坡地下水丰富的突出特点,提出了抗滑桩支挡与集水井联合井内仰斜排水孔疏排地下水并重的治理方案。治理工程竣工后,评估了井孔联合疏排地下水措施的排水效果,证明排水效果良好。

    Abstract:

    Taking the landslide control project of landslide No.13 at Panzhihua airport as an example, this paper briefly describes the basic situation of the landslide and focuses on the hydrogeological conditions of the study area. The rainy season rainfall accounts for 95% of the annual rainfall in the study area, and the occurrence times of moderate to heavy rain and rainfall days of 3 days or more are concentrated in the rainy season from July to September, accounting for more than 95% of the total. The rainfall in the study area is characterized by high intensity and concentration during the rainy season. Geophysical exploration and drilling revealed that the ground water in the field filling area at the rear edge of the landslide was abundant, with a "nest" -shaped discontinuous distribution and obvious stratification. Aquifers are characterized by high clay content, good water-bearing properties, poor pore connectivity, and poor drainage, making it difficult to dissipate quickly. Based on the prominent feature of abundant groundwater in the landslide area, a remediation scheme combining anti-slide piles and joint drainage by well and inclined drainage holes is proposed. After the completion of the treatment project, the drainage effect of the joint drainage measures by well and drainage hole was evaluated, and the practical results demonstrated excellent drainage effectiveness.

  • 图  1   地形地貌

    Figure  1.   The topography and landform

    图  2   典型工程地质断面

    Figure  2.   The typical engineering geology cross-section

    图  3   坡脚基岩露头

    Figure  3.   Outcrop of bedrock at the slope toe

    图  4   滑坡全貌[14]

    Figure  4.   Overall view of the landslide[14]

    图  5   钻孔(a)、桩坑(b)中揭露滑面

    Figure  5.   Exposed sliding surfaces in boreholes (a) and pile pits (b)

    图  6   2007—2019年年降水量分布图

    Figure  6.   Distribution map of annual average rainfall from 2007 to 2019

    图  7   2007—2019年月平均降水量分布图

    Figure  7.   Distribution map of monthly average rainfall from 2007 to 2019

    图  8   2010—2019年中雨及以上次数、连续3 d降雨次数分布图

    Figure  8.   Distribution map of the frequency of moderate rain or more for consecutive 3-days rainfall events from 2010 to 2019

    图  9   典型剖面物探成果

    Figure  9.   Typical section geophysical survey results

    图  10   坡脚、平台水沟地下水出露

    Figure  10.   The underground water emergence from slope foot, platform ditch

    图  11   一级马道监测点累计位移/沉降-时间曲线

    Figure  11.   Cumulative displacement/settlement - time curve of level 1 monitoring point

    图  12   滑坡区地层结构示意

    Figure  12.   Schematic diagram of strata structure in the landslide area

    图  13   滑坡治理平面布置简图

    Figure  13.   Schematic diagram of landslide control layout

    图  14   典型工程治理断面图

    Figure  14.   The cross-section of typical engineering governance

    图  15   集水井横断面布置图

    Figure  15.   The cross section layout of water collection wells

    图  16   累计位移(沉降)—时间曲线

    Figure  16.   Accumulated displacement (settlement) - date curve

    图  17   集水井出水口(左:出水口1;右:出水口2)

    Figure  17.   The collection well outlet (left: water outlet 1; right: water outlet 2)

    图  18   排水量—降水量—时间曲线(出口1)

    Figure  18.   Water inflow − rainfall − time curve (outlet 1)

    图  19   排水量—降水量—日期曲线(出口2)

    Figure  19.   Water inflow − rainfall − time curve (outlet 2)

    表  1   治理前后稳定性评估结果

    Table  1   Stability assessment results before and after treatment

    序号 断面
    编号
    治理前稳定系数 应急刷
    体积/m3
    设支挡结构后增加
    抗滑力/(kN·m−1
    设集水井后地下水
    降低高度/m
    治理后稳定系数
    自然工况 暴雨工况 地震工况 自然工况 暴雨工况 地震工况
    1 1-1' 1.03 1.00 0.86 23516 1740 5.8 1.35 1.31 1.25
    2 2-2' 1.03 1.00 0.85 2730 6.5 1.34 1.33 1.26
    3 3-3' 1.02 0.99 0.82 2609 7.2 1.35 1.32 1.26
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  • 收稿日期:  2023-06-14
  • 修回日期:  2024-01-07
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