砂泥岩互层地基防渗措施渗控效果及敏感性分析

温立峰, 孙少博, 李炎隆, 王民侠, 张晨, 田欣. 砂泥岩互层地基防渗措施渗控效果及敏感性分析[J]. 水文地质工程地质, 2025, 52(3): 163-173. doi: 10.16030/j.cnki.issn.1000-3665.202312023
引用本文: 温立峰, 孙少博, 李炎隆, 王民侠, 张晨, 田欣. 砂泥岩互层地基防渗措施渗控效果及敏感性分析[J]. 水文地质工程地质, 2025, 52(3): 163-173. doi: 10.16030/j.cnki.issn.1000-3665.202312023
WEN Lifeng, SUN Shaobo, LI Yanlong, WANG Minxia, ZHANG Chen, TIAN Xin. Seepage control effect and sensitivity analysis of anti-seepage measures for sand-mudstone interbedded foundation[J]. Hydrogeology & Engineering Geology, 2025, 52(3): 163-173. doi: 10.16030/j.cnki.issn.1000-3665.202312023
Citation: WEN Lifeng, SUN Shaobo, LI Yanlong, WANG Minxia, ZHANG Chen, TIAN Xin. Seepage control effect and sensitivity analysis of anti-seepage measures for sand-mudstone interbedded foundation[J]. Hydrogeology & Engineering Geology, 2025, 52(3): 163-173. doi: 10.16030/j.cnki.issn.1000-3665.202312023

砂泥岩互层地基防渗措施渗控效果及敏感性分析

  • 基金项目: 国家自然科学基金项目(U2443230;52479132);陕西省教育厅科研计划项目 (23JP113)
详细信息
    作者简介: 温立峰(1989—),男,博士,副教授,博士生导师,主要从事高堆石坝安全评价与变形控制相关的研究工作。E-mail:wenlifeng@xaut.edu.cn
  • 中图分类号: TV223.6

Seepage control effect and sensitivity analysis of anti-seepage measures for sand-mudstone interbedded foundation

  • 砂泥岩互层岩体是一种典型的复杂地质条件,其渗流场分布规律复杂,且传统渗流分析方法难以准确描述该规律。文章提出砂泥岩互层地基等效渗流场计算方法,揭示砂泥岩互层地基渗流场分布规律及不同渗控方案对其的影响。首先根据砂泥岩互层地基构造特点,提出基于土体分层渗流的砂泥岩互层地基等效渗流场计算方法;进而基于砂泥岩互层地基上的普化水库工程,建立反映工程区地质条件、枢纽布置和防渗措施的三维渗流场有限元计算模型;并讨论了砂泥岩互层岩体渗透各向异性对渗流场的影响,分析了不同防渗帷幕深度和长度组合方案对砂泥岩互层地基渗流场的控制效果。研究表明:(1)帷幕未完全截断透水层时,加深防渗帷幕深度可以明显降低坝基及两岸山体渗流量,使两岸山体溢出点渗透坡降逐渐减小,而使坝基部位和防渗帷幕的渗透坡降逐渐增加;(2)延长防渗帷幕长度可以降低两岸山体渗流量和渗透坡降,且帷幕长度增加只对帷幕加长侧渗流场产生较大的影响,但是随着帷幕长度进一步增加,对防渗效果提升的作用逐渐减弱;(3)砂泥岩互层地基渗流呈现各向异性特点,通过设置合理的防渗帷幕深度和长度可以有效控制地基的渗流量。研究成果可为砂泥岩互层地基的渗流控制提供理论参考。

  • 加载中
  • 图 1  砂泥岩互层渗流示意图

    Figure 1. 

    图 2  工程枢纽布置图

    Figure 2. 

    图 3  坝轴线工程地质剖面图

    Figure 3. 

    图 4  有限元计算模型

    Figure 4. 

    图 5  钻孔实测和反演计算水位对比

    Figure 5. 

    图 6  典型剖面水头等值线图

    Figure 6. 

    图 7  渗流量随帷幕深度变化规律

    Figure 7. 

    图 8  渗透坡降随帷幕深度变化规律

    Figure 8. 

    图 9  渗流量随左岸帷幕长度变化规律

    Figure 9. 

    图 10  渗透坡降随左岸帷幕长度变化规律

    Figure 10. 

    图 11  渗流量随右岸帷幕长度变化规律

    Figure 11. 

    图 12  渗透坡降随右岸帷幕长度变化规律

    Figure 12. 

    表 1  等效渗透系数取值范围与反演值

    Table 1.  Value range and inversion value of permeability coefficient of each part

    岩层岩层产状顺层渗透性切层渗透性
    渗透率/Lu等效渗透系数
    /(m·s−1
    反演渗透系数
    /(m·s−1
    渗透率/Lu等效渗透系数
    /(m·s−1
    反演渗透系数
    /(m·s−1
    强风化层砂岩各向异性>1008.31×10−6~6.59×10−55.17×10−5>1005.16×10−6~3.55×10−52.12×10−5
    泥岩各向异性>30>22
    弱风化层砂岩各向异性>1006.70×10−7~3.24×10−61.40×10−6>1001.53×10−7~0.67×10−68.30×10−7
    泥岩各向异性5.73~23.603.51~7.98
    微新岩层砂岩各向异性2.87~12.604.59×10−7~9.73×10−76.25×10−71.18~3.540.36×10−7~4.93×10−71.20×10−7
    泥岩各向异性0.77~2.180.21~1.53
    下载: 导出CSV

    表 2  计算工况

    Table 2.  Load cases

    计算工况工况编号防渗帷幕方案
    深度两岸长度
    设计帷幕布置方案工况1嵌入相对3 Lu线以下5 m左岸100 m,右岸70 m
    帷幕深度敏感性分析工况2—4加深5,10,20 m左岸100 m,右岸70 m
    左岸帷幕长度敏感性分析工况5—9加深10 m左岸延长20,40,60,80,100 m
    右岸帷幕长度敏感性分析工况10—14加深10 m右岸延长10,20,30,40,50 m
    下载: 导出CSV
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出版历程
收稿日期:  2023-12-17
修回日期:  2024-03-09
刊出日期:  2025-05-15

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