高海拔地区宽级配泥石流冲击拦砂坝试验研究

何胜庆, 郑达, 张文. 高海拔地区宽级配泥石流冲击拦砂坝试验研究[J]. 水文地质工程地质, 2024, 51(1): 123-134. doi: 10.16030/j.cnki.issn.1000-3665.202211009
引用本文: 何胜庆, 郑达, 张文. 高海拔地区宽级配泥石流冲击拦砂坝试验研究[J]. 水文地质工程地质, 2024, 51(1): 123-134. doi: 10.16030/j.cnki.issn.1000-3665.202211009
HE Shengqing, ZHENG Da, ZHANG Wen. Experimental study on the impact of wide graded debris flow on check dam in high altitude area[J]. Hydrogeology & Engineering Geology, 2024, 51(1): 123-134. doi: 10.16030/j.cnki.issn.1000-3665.202211009
Citation: HE Shengqing, ZHENG Da, ZHANG Wen. Experimental study on the impact of wide graded debris flow on check dam in high altitude area[J]. Hydrogeology & Engineering Geology, 2024, 51(1): 123-134. doi: 10.16030/j.cnki.issn.1000-3665.202211009

高海拔地区宽级配泥石流冲击拦砂坝试验研究

  • 基金项目: 西藏自治区自然资源厅项目(藏财采[2020]0890-1);成都理工大学地质灾害防治与地质环境保护国家重点实验室自主研究课题(SKLGP2020Z008)
详细信息
    作者简介: 何胜庆(1999—),男,硕士研究生,主要从事岩土工程方面的研究。E-mail:2486681236@qq.com
    通讯作者: 郑达(1977—),男,博士,教授,主要从事地质灾害评价防治及高边坡稳定性教学与研究工作。E-mail:da.zheng@cdut.edu.cn
  • 中图分类号: TV144;P642.23

Experimental study on the impact of wide graded debris flow on check dam in high altitude area

More Information
  • 在高海拔地区,由于山高谷深,坡表物质受物理风化严重,物源级配宽度范围大,泥石流的发育频率高,冲击力大,导致拦砂坝损毁严重。为研究高海拔地区宽级配泥石流对拦砂坝的冲击规律,以西藏地区发育的泥石流为原型,建立宽级配泥石流冲击拦砂坝的物理试验模型,选取泥石流容重、水槽坡度与泥石流固相最大粒径为变量,进行27组水槽试验,研究冲击力特征。结果表明:(1)宽级配泥石流在冲击拦砂坝过程中经历“冲击爬高、旋滚回流、堆积回淤”3个接触演化阶段,泥石流容重越小,爬高越大,冲淤过程的阶段性表现越明显;(2)拦砂坝的坝前冲击力随宽级配泥石流容重的增大而减小,在相同坡度和级配的条件下,容重越大,水流携带固体物源运动越困难,泥石流流速降低,泥石流的冲击力减小;(3)拦砂坝的坝前冲击力随沟槽坡度增大而增大,沟槽坡度越大,宽级配泥石流的流速和流深越大,泥石流冲击力就越大,并且泥石流固相粒径越大,坡度对冲击力的影响效果越明显;(4)拦砂坝的坝前冲击力随宽级配泥石流固相最大粒径增大而增大,且变化趋势较泥石流容重及沟槽坡度条件改变时更加显著,最大粒径与泥石流流速、流深没有明显规律关系。研究成果将为宽级配泥石流防治和研究提供一定的数据参考。

  • 加载中
  • 图 1  区内典型沟道物源

    Figure 1. 

    图 2  泥石流重度分布频数直方图

    Figure 2. 

    图 3  区内拦砂坝受冲击破坏损毁

    Figure 3. 

    图 4  泥石流水槽试验装置

    Figure 4. 

    图 5  拦砂坝模型参数

    Figure 5. 

    图 6  试验土样粒径累计曲线

    Figure 6. 

    图 7  容重1400 kg/m3、沟槽坡度17°泥石流过坝特征

    Figure 7. 

    图 8  容重1600 kg/m3、沟槽坡度17°泥石流过坝特征

    Figure 8. 

    图 9  容重1800 kg/m3、沟槽坡度17°泥石流过坝特征

    Figure 9. 

    图 10  泥石流容重对坝前冲击力的影响

    Figure 10. 

    图 11  泥石流容重改变时坝前冲击力的变化率

    Figure 11. 

    图 12  19°沟槽坡度泥石流容重与其他特征参数的关系

    Figure 12. 

    图 13  沟槽坡度对坝前冲击力的影响

    Figure 13. 

    图 14  沟槽坡度改变时坝前冲击力的变化率

    Figure 14. 

    图 15  1600 kg/m3容重条件沟槽坡度与泥石流特征参数的关系

    Figure 15. 

    图 16  最大粒径对坝前冲击力的影响

    Figure 16. 

    图 17  最大粒径改变时坝前冲击力的变化率

    Figure 17. 

    图 18  1600 kg/m3容重条件最大粒径与泥石流特征参数的关系

    Figure 18. 

    表 1  试验组次设计

    Table 1.  Design of experimental groups

    序号 颗粒级配 泥石流容重/(kg·m−3 沟槽坡度/(°) 试验次数
    1 清水 1000 17,19,21 3
    2 最大粒径40 mm 1400,1600,1800 17,19,21 9
    3 最大粒径30 mm 1400,1600,1800 17,19,21 9
    4 最大粒径20 mm 1400,1600,1800 17,19,21 9
    下载: 导出CSV

    表 2  试验结果

    Table 2.  Summary of experimental results

    组号 容重/
    (kg·m−3
    坡度/
    (°)
    最大粒径/
    mm
    流速/
    (m·s−1
    流深/
    cm
    弗洛德数
    平均冲击力/
    kPa
    1 1400 17 20 3.08 2.90 5.91 15.08
    2 1400 17 30 2.98 4.10 4.80 30.30
    3 1400 17 40 3.12 3.50 5.44 45.58
    4 1400 19 20 3.38 2.90 6.52 10.50
    5 1400 19 30 3.53 3.40 6.29 30.71
    6 1400 19 40 3.87 3.50 6.80 76.03
    7 1400 21 20 3.58 4.10 5.85 25.91
    8 1400 21 30 3.93 3.50 6.95 42.06
    9 1400 21 40 4.07 5.00 6.01 86.73
    10 1600 17 20 2.03 2.90 3.90 8.65
    11 1600 17 30 2.24 3.60 3.86 24.41
    12 1600 17 40 2.07 2.90 3.97 37.59
    13 1600 19 20 2.40 3.20 4.41 11.32
    14 1600 19 30 2.76 4.00 4.53 25.09
    15 1600 19 40 2.47 3.60 4.28 70.68
    16 1600 21 20 2.93 3.60 5.10 23.22
    17 1600 21 30 3.33 3.80 5.65 28.95
    18 1600 21 40 3.64 4.50 5.67 82.35
    19 1800 17 20 1.89 2.80 3.69 5.53
    20 1800 17 30 2.31 2.20 5.08 19.59
    21 1800 17 40 2.89 3.10 5.36 28.56
    22 1800 19 20 2.05 2.50 4.26 7.90
    23 1800 19 30 2.18 3.10 4.07 17.90
    24 1800 19 40 1.92 4.00 3.15 35.25
    25 1800 21 20 2.35 3.30 4.28 9.25
    26 1800 21 30 2.45 3.10 4.60 19.53
    27 1800 21 40 2.47 3.30 4.50 63.81
    下载: 导出CSV
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出版历程
收稿日期:  2022-11-03
修回日期:  2023-02-24
录用日期:  2023-02-24
刊出日期:  2024-01-15

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