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不同流量条件下红黏土地区地下管道断裂渗漏致塌半物理模型试验

王凯,  李麟玮,  向喜琼,  张勇,  安友豪,  安廷齐

王凯,李麟玮,向喜琼,等. 不同流量条件下红黏土地区地下管道断裂渗漏致塌半物理模型试验[J]. 地质科技通报,2026,45(5):1-13 doi: 10.19509/j.cnki.dzkq.tb20250298
引用本文: 王凯,李麟玮,向喜琼,等. 不同流量条件下红黏土地区地下管道断裂渗漏致塌半物理模型试验[J]. 地质科技通报,2026,45(5):1-13 doi: 10.19509/j.cnki.dzkq.tb20250298
WANG Kai,LI Linwei,XIANG Xiqiong,et al. Semi-physical model tests of collapses induced by leakage from fractured underground pipelines in red clay areas under different flow rate conditions[J]. Bulletin of Geological Science and Technology,2026,45(5):1-13 doi: 10.19509/j.cnki.dzkq.tb20250298
Citation: WANG Kai,LI Linwei,XIANG Xiqiong,et al. Semi-physical model tests of collapses induced by leakage from fractured underground pipelines in red clay areas under different flow rate conditions[J]. Bulletin of Geological Science and Technology,2026,45(5):1-13 doi: 10.19509/j.cnki.dzkq.tb20250298

不同流量条件下红黏土地区地下管道断裂渗漏致塌半物理模型试验

doi: 10.19509/j.cnki.dzkq.tb20250298
基金项目: 国家自然科学基金项目(42367022);贵州省科技计划项目(黔科合基础-ZK[2023]一般066;黔科合支撑[2023]一般127);国家重点研发计划(2022YFC3003301);贵州大学引进人才科研项目(贵大人基合字(2021)36号;贵大人基合字(2021)39号)
详细信息
    作者简介:

    王凯:E-mail:18275119736@163.com

    通讯作者:

    E-mail:lwli@gzu.edu.cn

  • 中图分类号: P642.26

Semi-physical model tests of collapses induced by leakage from fractured underground pipelines in red clay areas under different flow rate conditions

More Information
  • 摘要:

    红黏土地区由地下管道断裂渗漏诱发的地面塌陷灾害频发,严重威胁城市公共安全,造成生命与财产损失。现有管道渗漏致塌模型试验多针对砂土、粉土开展,针对红黏土介质,不同管道流量控制下的塌陷演化机理仍有待深入。以贵州红黏土为研究对象,开展 6 组不同管道流量的半结构化物理模型试验,固定管道全断面断裂模式与覆盖层厚度;综合采用高速相机、土压力传感器、孔隙水压力传感器、激光位移计开展全过程监测,获取土体宏观变形破坏、湿润锋运移、土压力−孔隙水压力响应以及地表位移演化特征。在管道断裂条件保持一致时,管道流量减小会削弱渗漏水流对土体的掏蚀搬运能力,土体侵蚀速率降低,湿润锋运移机制发生转变,土洞优势发育方向由水平转向竖向,发生塌陷的临界覆盖层厚度随之降低;当流量低于临界值时,仅发育土洞而不会发生地面塌陷。管道流量较高工况无明显土拱效应,小管道流量工况土洞发育过程可形成显著土拱效应;塌陷发生前地表位移微弱,灾害表现出较强隐蔽性;不同管道流量下发生塌陷的工况,致塌模式均为渗漏水流顶破上覆土层。同时,随管道流量改变,孔隙水压力优先响应的监测点位随湿润锋扩展方向发生转换。本研究揭示了红黏土介质中管道流量对土洞演化、应力渗流响应及致塌模式的控制机理,可为城市地下管道全生命周期安全监测、地面塌陷风险预警及工程防控方案制定提供理论依据。

     

  • 图 1  红黏土地区管道渗漏诱发地面塌陷示意图

    Figure 1.  Schematic diagram of ground collapse induced by pipeline leakage in red clay areas

    图 2  半结构化物理模型试验装置

    Figure 2.  Setup of semi-structured physical model test

    图 3  监测设备布置示意图

    Figure 3.  Schematic diagram of monitoring equipment arrangement

    图 4  不同管道流量工况下半物理模型宏观变形破坏特征

    a1~f1. 土体湿润;a2~f2. 土洞形成;a3~f3. 土洞发育;a4~e4,a5~e5. 塌陷发生;f4,f5. 土洞稳定。红色虚线为土洞边界;工况1~6管道流量见表2,下同

    Figure 4.  Macroscopic deformation and failure characteristics of semi-physical model under different pipe flow rate conditions

    图 5  不同管道流量工况下土体湿润锋演化特征(a~c. 工况1~3;d~f. 工况4~6。蓝色虚线为土体湿润锋边界)

    Figure 5.  Evolution characteristics of soil mass wetting front under different pipe flow rate conditions

    图 6  不同工况条件下土压力变化曲线

    Ⅰ~Ⅳ代表物理模型宏观变形破坏4个阶段,分别为土体湿润、土洞形成、土洞发育和塌陷发生(土洞稳定),其中工况1~5第Ⅳ阶段为塌陷发生,工况6第Ⅳ阶段为土洞稳定,见图4;S1~S6为土压力传感器编号;下同

    Figure 6.  Variation curves of soil pressure under different working conditions

    图 7  不同工况条件下孔隙水压力变化曲线(P1,P2为孔隙水压力传感器编号)

    Figure 7.  Variation curves of pore water pressure under different working conditions

    图 8  不同工况条件下地表位移变化曲线(D1,D2为激光位移传感器编号)

    Figure 8.  Variation curves of surface displacement under different working conditions

    图 9  覆盖层顶破型塌陷模式示意图

    Figure 9.  Schematic diagram of overburden-breaching collapse mode

    图 10  不同工况下土洞尺寸及塌陷坑范围

    Figure 10.  Soil cavity size and collapse pit extent under different working conditions

    表  1  红黏土物理力学参数

    Table  1.   Physical and mechanical parameters of red clay

    天然密度/
    (g·cm−3)
    干密度/
    (g·cm−3)
    含水
    率/%
    液限/
    %
    塑限/
    %
    黏聚
    力/kPa
    内摩擦
    角/(°)
    渗透系数/
    (10−6m·s−1)
    1.87 1.48 25.7 39.7 15.7 30.2 10.2 8.33
    下载: 导出CSV

    表  2  模型试验方案

    Table  2.   Model test schemes

    试验工况
    名称
    管道流量/
    (m3·h−1)
    覆盖层
    厚度/cm
    管道断裂
    间距/cm
    管道破坏
    方式
    工况1 13.0 12 1 全断面断裂
    工况2 11.8
    工况3 10.6
    工况4 9.4
    工况5 8.2
    工况6 7.0
    下载: 导出CSV
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  • 收稿日期:  2025-06-30
  • 录用日期:  2025-11-14
  • 修回日期:  2025-11-14
  • 网络出版日期:  2025-11-18

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