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含优势渗流层边坡降雨入渗下的可靠度分析

肖景红 王敏 王川 冷先伦

肖景红, 王敏, 王川, 冷先伦. 含优势渗流层边坡降雨入渗下的可靠度分析[J]. 地质科技通报, 2021, 40(6): 193-204. doi: 10.19509/j.cnki.dzkq.2021.0619
引用本文: 肖景红, 王敏, 王川, 冷先伦. 含优势渗流层边坡降雨入渗下的可靠度分析[J]. 地质科技通报, 2021, 40(6): 193-204. doi: 10.19509/j.cnki.dzkq.2021.0619
Xiao Jinghong, Wang Min, Wang Chuan, Leng Xianlun. Reliability analysis of slope with dominant seepage interlayer under rainfall infiltration[J]. Bulletin of Geological Science and Technology, 2021, 40(6): 193-204. doi: 10.19509/j.cnki.dzkq.2021.0619
Citation: Xiao Jinghong, Wang Min, Wang Chuan, Leng Xianlun. Reliability analysis of slope with dominant seepage interlayer under rainfall infiltration[J]. Bulletin of Geological Science and Technology, 2021, 40(6): 193-204. doi: 10.19509/j.cnki.dzkq.2021.0619

含优势渗流层边坡降雨入渗下的可靠度分析

doi: 10.19509/j.cnki.dzkq.2021.0619
基金项目: 

国家重点研发计划 2017YFF0108705

详细信息
    作者简介:

    肖景红(1980-), 男, 高级工程师, 主要从事隧道及边坡施工安全控制方面的研究。E-mail:22927082@qq.com

    通讯作者:

    冷先伦(1980-), 男, 副研究员, 主要从事岩土力学与岩土工程稳定方面的研究。E-mail:xlleng@whrsm.ac.cn

  • 中图分类号: X43

Reliability analysis of slope with dominant seepage interlayer under rainfall infiltration

  • 摘要: 含优势渗流层边坡在降雨入渗的作用下其渗流场往往具有较高的不确定性,这给边坡的稳定性评价带来困难,通常采用概率的方法解决此类问题。针对含优势渗流层边坡降雨入渗下的可靠度问题,通过将应力分析中的点估计-有限元法引入到边坡渗流-稳定性分析,提出了考虑优势渗流层渗透特性不确定性的渗流概率分析和边坡可靠度分析方法;其次以广西某含碎石夹层土坡为例,分析了降雨入渗下碎石夹层的优势渗流效应及渗流概率,并基于此开展了该边坡降雨入渗下的可靠度分析。结果表明:①含优势渗流层边坡雨水沿优势渗流层渗入坡体内部的深度显著高于沿坡面渗入的深度;优势渗流层渗透特性的不确定性对渗流结果的影响较大,使得边坡稳定性分析具有较强的不确定性;②随着雨水入渗持时的增加,含优势渗流层边坡不同滑动面的失效概率总体呈现增加趋势,最危险滑动面的位置不断向边坡下部演化;依托工程滑动面位置的预测结果与工程实际吻合;③提出的概率分析方法适用于分析含优势渗流层边坡降雨入渗影响下的稳定性问题,而且具有计算量小的优势,可作这类边坡可靠度分析的一种新方法。

     

  • 图 1  含优势渗流层边坡概化模型

    Figure 1.  Generalized model of slope with dominant seepage interlayer

    图 2  基于优势渗流层渗流概率的边坡可靠度分析流程

    Figure 2.  Analysis process of slope reliability using seepage probability of dominant permeable layer

    图 3  边坡几何模型

    Figure 3.  Model of slope geometry

    图 4  边坡优势渗流层渗流参数的随机数取值及统计分布

    Figure 4.  Random number values and statistical distribution of seepage parameters of dominant seepage interlayer of the slope

    图 5  湿润锋深度的统计规律及对比分析

    Figure 5.  Statistical and comparative analysis of the wet fronts depth

    图 6  边坡安全系数的统计规律及对比分析

    Figure 6.  Statistical and comparative analysis of safety factors of the slope

    图 7  依托工程边坡地质剖面

    Figure 7.  Geological section of the slope of the engineering case

    图 8  依托工程滑坡概况

    Figure 8.  Overview of the landslide of the engineering case

    图 9  边坡渗流分析的材料参数

    Figure 9.  Material parameters for slope seepage analysis

    图 10  边坡潜在滑动面的设置

    Figure 10.  Setting of potential sliding surfaces of the slope

    图 11  降雨入渗下边坡含水量分布图

    Figure 11.  Water content distribution of the slope under rainfall infiltration

    图 12  优势渗流层含水量的概率分布示意图

    Figure 12.  Probability distribution of water content of the dominant seepage interlayer of the slope

    图 13  不同滑动面安全系数随降雨持时的概率分布规律

    Figure 13.  Probability distribution of safety factors of different sliding surfaces with rainfall duration

    图 14  边坡稳定性可靠度随降雨持时的变化规律

    Figure 14.  Variation of reliability of slope stability with rainfall duration

    表  1  边坡地层的水力和力学参数

    Table  1.   Hydraulic and mechanical parameters of slope formation

    地层类型 渗流计算的参数 稳定性计算的参数
    残余体积含水量/(m3·m-3) 饱和体积含水量/(m3·m-3) 饱和渗透系数/(m·d-1) a m n 干密度/(g·cm-3) 黏聚力/kPa 内摩擦角/(°)
    常规地层 0.10 0.45 0.05 15 1.8 0.7 1.3 45 35
    优势渗流层 0.08±0.02(x±σx) 0.5±0.1 (x±σx) 1.0±0.3 (x±σx) 25 1.0 1.3 1.5 35 45
    注:anm为控制体积水含量函数形状的曲线拟合参数
    下载: 导出CSV

    表  2  坡体岩土力学参数

    Table  2.   Geotechnical mechanics parameters of the slope

    地层类型 密度/(g·cm-3) 黏聚力/kPa 内摩擦角/(°) 体积含水量/(m3·m-3)
    天然 饱和 天然 饱和 天然 饱和 天然 残余 饱和
    碎石夹层 1.7 1.9 36 25 44 35 0.12 0.08 0.54
    粉质黏土 1.4 1.6 45 33 37 26 0.15 0.10 0.46
    下载: 导出CSV

    表  3  边坡渗流拟合的输入参数

    Table  3.   Input parameters for slope seepage fitting

    土体类型 残余体积含水量/(m3·m-3) 饱和体积含水量/(m3·m-3) 饱和渗透系数/(m·d-1) a m n
    粉质黏土 0.10 0.45 0.05 15 1.8 0.7
    碎石夹层 0.08±0.01(x±σx) 0.54±0.07(x±σx) 1.0±0.3(x±σx) 25 1.0 1.3
    下载: 导出CSV
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