近水平层状坝基岩体渗透结构及其工程意义

王俊智, 李清波, 王贵军, 张一. 近水平层状坝基岩体渗透结构及其工程意义[J]. 水文地质工程地质, 2022, 49(1): 12-19. doi: 10.16030/j.cnki.issn.1000-3665.202105024
引用本文: 王俊智, 李清波, 王贵军, 张一. 近水平层状坝基岩体渗透结构及其工程意义[J]. 水文地质工程地质, 2022, 49(1): 12-19. doi: 10.16030/j.cnki.issn.1000-3665.202105024
WANG Junzhi, LI Qingbo, WANG Guijun, ZHANG Yi. Permeability structure of the horizontally-stratified dam foundation rock mass and its engineering significance[J]. Hydrogeology & Engineering Geology, 2022, 49(1): 12-19. doi: 10.16030/j.cnki.issn.1000-3665.202105024
Citation: WANG Junzhi, LI Qingbo, WANG Guijun, ZHANG Yi. Permeability structure of the horizontally-stratified dam foundation rock mass and its engineering significance[J]. Hydrogeology & Engineering Geology, 2022, 49(1): 12-19. doi: 10.16030/j.cnki.issn.1000-3665.202105024

近水平层状坝基岩体渗透结构及其工程意义

  • 基金项目: 国家自然科学基金项目(41902245);国家重点研发计划项目(2018YFC1508703);河南省重点研发与推广专项科技攻关项目(212102311150);黄河勘测规划设计研究院有限公司自主研发项目
详细信息
    作者简介: 王俊智(1987-),男,博士,高级工程师,主要从事水文地质的研究。E-mail:wang_jzh@yrec.cn
    通讯作者: 李清波(1964-),男,本科,正高级工程师,主要从事工程地质及水文地质的研究。E-mail:liqb_yrec@163.com
  • 中图分类号: P641.2; TV698

Permeability structure of the horizontally-stratified dam foundation rock mass and its engineering significance

More Information
  • 查明坝基岩体的渗透结构对于大坝工程防渗方案的制定具有重要意义。以黄河古贤水利枢纽工程近水平分布的红层坝基岩体为研究对象,使用“连续、高分辨率”压水试验数据处理与统计方法,分析了岩体透水率与高程、岩性及顺层剪切带的关系,阐明了坝基岩体的渗透结构,提出了工程防渗建议。研究发现,坝基岩体渗透结构表现出结构性和随机性双重特征。结构性表现为岩体透水率随高程的降低而减小;随机性表现为岩体透水率会因岩性和剪切构造等随机变化。对于河床及滩地坝基岩体,风化卸荷带底高程在450 m附近,1 Lu关键透水率指标界线的底高程位于340 m附近。对于岸坡坝基岩体,3 Lu关键透水率指标界线的底高程位于560~580 m。在坝基勘察深度范围内,350~360 m高程段连续分布具有一定厚度的软岩类岩体,剪切构造不发育且岩体透水微弱,可视为相对隔水层,对坝基防渗帷幕优化设计具有指示意义。文章提出的统计、分析方法具有一定普适性,可为类似工程所借鉴。

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  • 图 1  黄河古贤水利枢纽工程重力坝坝轴线地质剖面示意图

    Figure 1. 

    图 2  坝址区压水试验钻孔分布位置示意图

    Figure 2. 

    图 3  坝址区坝基岩体透水率概率图

    Figure 3. 

    图 4  河床及滩地岩体透水率平均值随高程变化

    Figure 4. 

    图 5  岸坡岩体透水率平均值随高程变化

    Figure 5. 

    图 6  河床及滩地岩体透水率与岩性、剪切带关系

    Figure 6. 

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出版历程
收稿日期:  2021-05-06
修回日期:  2021-07-10
刊出日期:  2022-01-15

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