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秦巴山区典型碎石土抗剪强度变化规律及其在堆积层滑坡机理分析中的应用

张昊天, 王新刚, 罗力, 王友林, 郭倩怡, 薛晨. 秦巴山区典型碎石土抗剪强度变化规律及其在堆积层滑坡机理分析中的应用[J]. 中国地质灾害与防治学报, 2024, 35(5): 50-58. doi: 10.16031/j.cnki.issn.1003-8035.202306038
引用本文: 张昊天, 王新刚, 罗力, 王友林, 郭倩怡, 薛晨. 秦巴山区典型碎石土抗剪强度变化规律及其在堆积层滑坡机理分析中的应用[J]. 中国地质灾害与防治学报, 2024, 35(5): 50-58. doi: 10.16031/j.cnki.issn.1003-8035.202306038
ZHANG Haotian, WANG Xingang, LUO Li, WANG Youlin, GUO Qianyi, XUE Chen. Changing law of shear strength of typical gravel soil in Qinba Mountain area and its application in the analysis of landslide mechanism in accumulation layers[J]. The Chinese Journal of Geological Hazard and Control, 2024, 35(5): 50-58. doi: 10.16031/j.cnki.issn.1003-8035.202306038
Citation: ZHANG Haotian, WANG Xingang, LUO Li, WANG Youlin, GUO Qianyi, XUE Chen. Changing law of shear strength of typical gravel soil in Qinba Mountain area and its application in the analysis of landslide mechanism in accumulation layers[J]. The Chinese Journal of Geological Hazard and Control, 2024, 35(5): 50-58. doi: 10.16031/j.cnki.issn.1003-8035.202306038

秦巴山区典型碎石土抗剪强度变化规律及其在堆积层滑坡机理分析中的应用

  • 基金项目: 国家重点研发计划项目(2023YFC3008401);陕西省自然科学基础研究计划重点项目(2024JC-ZDXM-19)
详细信息
    作者简介: 张昊天(1999—),男,硕士研究生,主要从事堆积层滑坡致滑机理研究。E-mail:1187910566@qq.com
    通讯作者: 王新刚(1984—),男,教授,博士生导师,主要从事地质灾害机理与防控研究。E-mail:xgwang@nwu.edu.cn
  • 中图分类号: P642.22

Changing law of shear strength of typical gravel soil in Qinba Mountain area and its application in the analysis of landslide mechanism in accumulation layers

More Information
  • 秦巴山区堆积层滑坡具有数量多、分布广、密度大和频次高的特点,常造成十分严重的灾害。文章以秦巴山区小岭镇岭丰村三组矿洞滑坡碎石土为研究对象,通过室内大型直剪试验对研究区碎石土进行了深入研究,探讨了不同含水率、不同干密度和不同法向应力下碎石土抗剪强度的变化规律,并基于室内试验成果采用Midas GTS NT有限元数值模拟软件对该滑坡发生前的边坡进行计算分析,模拟分析了该边坡在开挖后及开挖与降雨耦合两种工况下应力、位移和稳定性的变化情况,最后以此为依据总结了典型开挖诱发型堆积层滑坡的发生机理。通过数值模拟计算发现:人类工程活动即开挖坡脚和该地区出现的强降雨是导致滑坡的主要诱发因素;秦巴山区典型开挖诱发型滑坡的变形模式可被归纳为:牵引-蠕滑式。研究成果可为秦巴山区堆积层滑坡的防治提供一定参考。

  • 加载中
  • 图 1  岭丰村三组矿洞滑坡平面图

    Figure 1. 

    图 2  岭丰村三组矿洞滑坡(镜向:274°)

    Figure 2. 

    图 3  矿洞滑坡碎石土级配曲线

    Figure 3. 

    图 4  试验仪器及试验材料

    Figure 4. 

    图 5  相同干密度(ρd=1.4 g/cm3)、不同含水率下剪切应力与剪切位移变化曲线

    Figure 5. 

    图 6  相同干密度(ρd=1.4 g/cm3)、不同含水率下剪切应力峰值变化规律

    Figure 6. 

    图 7  相同干密度下(ρd=1.4 g/cm3)抗剪强度指标与含水率关系曲线

    Figure 7. 

    图 8  相同含水率(ω=10.6%)、不同干密度下剪切应力与剪切位移的变化规律

    Figure 8. 

    图 9  相同含水率(ω=10.6%)、不同干密度下剪切应力峰值变化规律

    Figure 9. 

    图 10  相同含水率(ω=10.6%)下抗剪强度指标与干密度关系曲线

    Figure 10. 

    图 11  Midas GTS NT有限元模型

    Figure 11. 

    图 12  开挖后滑坡位移云图

    Figure 12. 

    图 13  开挖前后滑坡最大剪应力云图

    Figure 13. 

    图 14  开挖前后塑性区分布图

    Figure 14. 

    图 15  开挖与降雨耦合作用后滑坡位移云图

    Figure 15. 

    图 16  开挖与降雨耦合作用后滑坡塑性分区图

    Figure 16. 

    表 1  本次试验方案

    Table 1.  Large-scale direct shear test program

    试样编号 含水率/% 干密度/(g·cm−3
    S01 5.0 1.5
    S02 10.6 1.5
    S03 15.0 1.5
    S04 19.4 1.5
    S05 5.0 1.4
    S06 10.6 1.4
    S07 15.0 1.4
    S08 19.4 1.4
    S09 5.0 1.4
    S10 10.6 1.3
    S11 15.0 1.3
    S12 19.4 1.3
    下载: 导出CSV

    表 2  数值模拟参数

    Table 2.  Numerical model parameters

    类型 重度
    /(kN·m−3
    泊松比 c/kPa φ/(°) E/MPa
    碎石土层 21.2 0.32 25.2 31.1 100
    滑带土(天然工况) 19.2 0.33 25.0 30.5 90
    滑带土(饱和工况) 19.7 0.40 20.9 19.6 70
    强风化层 23.3 0.30 50.0 35.0 200
    基岩层 24.5 0.28 428.0 38.0 1000
    下载: 导出CSV
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  • 文章访问数:  188
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出版历程
收稿日期:  2023-06-29
修回日期:  2024-04-03
录用日期:  2024-04-07
刊出日期:  2024-10-25

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