基于斜率模型的突发型黄土滑坡失稳时间预测

方汕澳, 许强, 修德皓, 赵宽耀, 李志刚, 蒲枫. 基于斜率模型的突发型黄土滑坡失稳时间预测[J]. 水文地质工程地质, 2021, 48(4): 169-179. doi: 10.16030/j.cnki.issn.1000-3665.202009012
引用本文: 方汕澳, 许强, 修德皓, 赵宽耀, 李志刚, 蒲枫. 基于斜率模型的突发型黄土滑坡失稳时间预测[J]. 水文地质工程地质, 2021, 48(4): 169-179. doi: 10.16030/j.cnki.issn.1000-3665.202009012
FANG Shan’ao, XU Qiang, XIU Dehao, ZHAO Kuanyao, LI Zhigang, PU Feng. A study of the predicted instability time of sudden loess landslides based on the SLO model[J]. Hydrogeology & Engineering Geology, 2021, 48(4): 169-179. doi: 10.16030/j.cnki.issn.1000-3665.202009012
Citation: FANG Shan’ao, XU Qiang, XIU Dehao, ZHAO Kuanyao, LI Zhigang, PU Feng. A study of the predicted instability time of sudden loess landslides based on the SLO model[J]. Hydrogeology & Engineering Geology, 2021, 48(4): 169-179. doi: 10.16030/j.cnki.issn.1000-3665.202009012

基于斜率模型的突发型黄土滑坡失稳时间预测

  • 基金项目: 国家自然科学基金重点项目(41630640);国家自然科学基金重大项目(41790445)
详细信息
    作者简介: 方汕澳(1997-),男,硕士研究生,主要从事地质灾害机理及防治方面研究。E-mail: 1026049600@qq.com
    通讯作者: 许强(1968-),男,博士,教授,博士生导师,主要从事地质灾害预测评价及防治处理方面的教学与研究工作。E-mail: xq@cdut.edu.cn
  • 中图分类号: P642.22

A study of the predicted instability time of sudden loess landslides based on the SLO model

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  • 突发型黄土滑坡灾前变形量小,加速阶段历时短,预警预报难度大。为探究该类滑坡失稳时间预测的新途径,降低滑坡造成的经济损失和人员伤亡,以2019年甘肃黑方台地区发生的4起滑坡为研究对象,基于改进的切线角模型确定滑坡变形阶段,提出以改进切线角为指标的简化累计计算方法;采用斜率模型(SLO模型)从滑坡各变形阶段起算进行失稳时间预测,从速度倒数变化趋势、滑坡成灾模式等方面分析预测结果差异。研究发现:(1)斜率模型在突发型黄土滑坡失稳时间预测方面具有一定的可行性,从80°切线角起算得到的预测精度最高;(2)以切线角为划分指标进行简化累计计算能降低数据波动对预测结果的影响,反映预测寿命变化趋势,提高预测精度;(3)速度倒数变化趋势呈“凹”型时提前预测概率大,速度倒数变化趋势呈“凸”型时滞后预测概率大,速度倒数变化趋势呈线性时模型预测精度较高;(4)该模型在黄土滑移崩塌型滑坡中的预测效果要优于静态液化型滑坡。

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  • 图 1  黑方台滑坡分布

    Figure 1. 

    图 2  滑坡监测点布设示意图

    Figure 2. 

    图 3  累计计算示意图

    Figure 3. 

    图 4  预测寿命图(据文献[22],有删改)

    Figure 4. 

    图 5  党川6#滑坡变形曲线

    Figure 5. 

    图 6  党川6#滑坡预测寿命

    Figure 6. 

    图 7  陈家6#和党川7#滑坡预测寿命

    Figure 7. 

    图 8  党川4#滑坡变形曲线

    Figure 8. 

    图 9  党川4#滑坡预测寿命

    Figure 9. 

    图 10  滑坡速度倒数曲线图

    Figure 10. 

    图 11  静态液化型滑坡成灾模式图(据文献[27],有删改)

    Figure 11. 

    图 12  滑移崩塌型滑坡成灾模式图(据文献[27],有删改)

    Figure 12. 

    表 1  2019年成功预警的滑坡

    Table 1.  Basic characteristics of landslides predicted in 2019

    编号 滑坡 发生时间 滑坡类型 提前预警时间
    1 陈家6# 2019-03-04 滑移崩塌型 2 h
    2 党川6# 2019-03-26 滑移崩塌型 40 min
    3 党川4# 2019-04-19 静态液化型 18 min
    4 党川7# 2019-10-05 滑移崩塌型 32 h
    下载: 导出CSV

    表 2  党川6#滑坡预测结果均方根误差

    Table 2.  RMSE of the predicted results of the Dangchuan 6# landslide

    起算角度 累计计算/h 简化累计计算/h
    60°起算 0.40 0.26
    65°起算 0.40 0.45
    70°起算 0.70 0.44
    75°起算 1.00 0.47
    80°起算 0.56 0.38
    下载: 导出CSV

    表 3  陈家6#和党川7#滑坡预测结果的均方根误差

    Table 3.  RMSE of the predicted results of the Chenjia 6# and Dangchuan 7# landslide

    滑坡 起算角度 累计计算/h 简化累计计算/h
    陈家6# 60°起算 10.54 5.22
    65°起算 20.64 2.08
    70°起算 3.15 1.49
    75°起算 3.29 2.68
    80°起算 2.36 0.07
    党川7# 60°起算 41.49 39.74
    65°起算 35.27 31.95
    70°起算 28.71 24.72
    75°起算 23.51 12.97
    80°起算 18.23 9.74
    下载: 导出CSV

    表 4  党川4#滑坡预测结果均方根误差

    Table 4.  Predicted RMSE of the Dangchuan 4# landslide

    起算角度 累计计算/h 简化累计计算/h
    60°起算 8.77 7.57
    65°起算 9.41 8.24
    70°起算 11.24 9.80
    75°起算 16.93 14.22
    80°起算 12.48 4.28
    下载: 导出CSV
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收稿日期:  2020-09-03
修回日期:  2020-11-04
刊出日期:  2021-07-15

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