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喜马拉雅中段冰湖终碛坝体溃决过程实验研究

苏鹏程, 刘威, 李昊, 陈乔, 刘阳, 张议芳. 喜马拉雅中段冰湖终碛坝体溃决过程实验研究——以嘉龙错冰湖终碛坝为例[J]. 中国地质灾害与防治学报, 2021, 32(5): 18-28. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-03
引用本文: 苏鹏程, 刘威, 李昊, 陈乔, 刘阳, 张议芳. 喜马拉雅中段冰湖终碛坝体溃决过程实验研究——以嘉龙错冰湖终碛坝为例[J]. 中国地质灾害与防治学报, 2021, 32(5): 18-28. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-03
SU Pengcheng, LIU Wei, LI Hao, CHEN Qiao, LIU Yang, ZHANG Yifang. Experimental study on the process of end-moraine dam failure in the middle Himalaya glacial lake: Taking the Jialongcuo glacial lake end-moraine dam as an example[J]. The Chinese Journal of Geological Hazard and Control, 2021, 32(5): 18-28. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-03
Citation: SU Pengcheng, LIU Wei, LI Hao, CHEN Qiao, LIU Yang, ZHANG Yifang. Experimental study on the process of end-moraine dam failure in the middle Himalaya glacial lake: Taking the Jialongcuo glacial lake end-moraine dam as an example[J]. The Chinese Journal of Geological Hazard and Control, 2021, 32(5): 18-28. doi: 10.16031/j.cnki.issn.1003-8035.2021.05-03

喜马拉雅中段冰湖终碛坝体溃决过程实验研究

  • 基金项目: 中国科学院西部青年学者项目;国家自然科学基金项目(41877261;U19A2049);中国地调局地质调查项目(DD20190637);西藏自治区自然资源厅防治能力体系建设项目(2020-0890-2);四川省2021年第一批重点研发基金项目(2021YFSY0036)
详细信息
    作者简介: 苏鹏程(1981-),男,安徽桐城人 ,博士,主要从事高速公路、水电基地及城镇地质灾害评估与工程减灾方面的研究工作。 E-mail:supengcheng@imde.ac.cn
  • 中图分类号: P642;TV131.61

Experimental study on the process of end-moraine dam failure in the middle Himalaya glacial lake: Taking the Jialongcuo glacial lake end-moraine dam as an example

  • 终碛坝广泛分布于世界各地的高山和极高山区。为了探究终碛坝的溃决过程,了解溃口的演变特征,文章以嘉龙错终碛坝的原位实验,模拟了终碛湖漫顶溃决过程。通过分析实验结果发现:(1)根据观察,将终碛坝溃决过程划分为坝体下游坡面冲刷、“溯源侵蚀”、出水口下切和溃口拓宽四个阶段。(2)上游湖区崩塌体激发的涌浪会造成溃口内的瞬时流量增加数倍,从而使得在有涌浪和无涌浪的条件下,“溯源侵蚀”过程出现陡坎和斜坡两种下切型。(3)通过分析溃口下切侵蚀过程,发现溃口的下切侵蚀发展过程主要受到坝体孔隙比和细粒含量的影响,并且溃口中点侵蚀率与水流剪应力存在一定的线性关系,符合线性侵蚀模型。通过分析发现,嘉龙错终碛坝的侵蚀系数为0.051,临界启动应力为237.64 Pa。与堰塞坝相比,可侵蚀系数比更小,而临界启动应力更大。

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  • 图 1  原位实验地理位置和局部背景图

    Figure 1. 

    图 2  坝体材料颗粒分部曲线

    Figure 2. 

    图 3  实验设备布置以及初始溃口形态(单位:m)

    Figure 3. 

    图 4  坝体形态图

    Figure 4. 

    图 5  WD为0.8 m时的库区水位变化曲线

    Figure 5. 

    图 6  两种形式的溃口下切过程

    Figure 6. 

    图 7  陡坎和斜坡在阶段二和阶段三的发展示意图

    Figure 7. 

    图 8  WD分别为0.8 m(斜坡)和0.4 m(陡坎)时的流量曲线

    Figure 8. 

    图 9  坝顶宽为0.2~0.8 m时的溃口深度变化曲线

    Figure 9. 

    图 10  WD为0.6 m时陡坎转化为斜坡的过程

    Figure 10. 

    图 11  坝顶宽分别为0.8 m和0.4 m时的溃口A点侵蚀率

    Figure 11. 

    图 12  WD为0.8 m时的溃口A点侵蚀率与水流剪应力关系

    Figure 12. 

    表 1  实验工况参数

    Table 1.  Experimental working conditions parameters

    实验
    编号
    汇水流量

    Qin
    /(L·s−1
    坝顶宽

    WD
    /m
    坝体下游
    坡度
    θ
    /(°)
    坝高

    HD
    /m
    黏聚力
    C/kPa
    内摩擦角
    φ/(°)
    天然
    含水率
    饱和天然
    含水率
    饱和
    12.5


    0.21∶1


    1


    17.43


    12.17


    27.97


    21.85


    20.4
    30.6
    40.8
    下载: 导出CSV

    表 2  关于kdτc的对比

    Table 2.  The comparison of kd and τc

    kdτc/Pa坝体类型文献
    0.051237.64终碛坝本文
    0.145819.6714人工堰塞坝[27]
    0.193.59人工堰塞坝[26]
    0.0849.11唐家山堰塞坝[26, 28]
    下载: 导出CSV
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出版历程
收稿日期:  2021-05-22
修回日期:  2021-07-26
刊出日期:  2021-10-25

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