三峡库区巫溪凤凰山危岩体失稳机理与碎屑流动力学特征

程什, 代贞伟, 付小林, 张安乐, 王鲁琦, 张晨阳, 杨龙伟, 蒋先念. 2023. 三峡库区巫溪凤凰山危岩体失稳机理与碎屑流动力学特征. 华南地质, 39(3): 470-481. doi: 10.3969/j.issn.2097-0013.2023.03.006
引用本文: 程什, 代贞伟, 付小林, 张安乐, 王鲁琦, 张晨阳, 杨龙伟, 蒋先念. 2023. 三峡库区巫溪凤凰山危岩体失稳机理与碎屑流动力学特征. 华南地质, 39(3): 470-481. doi: 10.3969/j.issn.2097-0013.2023.03.006
CHENG Shi, DAI Zhen-Wei, FU Xiao-Lin, ZHANG An-Le, WANG Lu-Qi, ZHANG Chen-Yang, YANG Long-Wei, JIANG Xian-Nian. 2023. Instability Mechanism and Debris Flow Dynamics of Fenghuang Mountain Dangerous Rock Mass in Wuxi, Three Gorges Reservoir Area. South China Geology, 39(3): 470-481. doi: 10.3969/j.issn.2097-0013.2023.03.006
Citation: CHENG Shi, DAI Zhen-Wei, FU Xiao-Lin, ZHANG An-Le, WANG Lu-Qi, ZHANG Chen-Yang, YANG Long-Wei, JIANG Xian-Nian. 2023. Instability Mechanism and Debris Flow Dynamics of Fenghuang Mountain Dangerous Rock Mass in Wuxi, Three Gorges Reservoir Area. South China Geology, 39(3): 470-481. doi: 10.3969/j.issn.2097-0013.2023.03.006

三峡库区巫溪凤凰山危岩体失稳机理与碎屑流动力学特征

  • 基金项目:

    湖北省自然科学基金项目(NO. 2020CFB352)、三峡后续工作地质灾害防治项目(NO. 0001212023CC60001、NO.00012120 21CC60001)

详细信息
    作者简介: 程什(2000—),男,硕士研究生,从事地质灾害动力学成灾机理研究,E-mail:852996115@qq.com
    通讯作者: 代贞伟(1986—),男,博士,高级工程师,从事地质灾害防灾减灾研究工作,E-mail:daizhenwei@mail.cgs.gov.cn
  • 中图分类号: P642.21

Instability Mechanism and Debris Flow Dynamics of Fenghuang Mountain Dangerous Rock Mass in Wuxi, Three Gorges Reservoir Area

More Information
    Corresponding author: DAI Zhen-Wei
  • 三峡库区巫溪县凤凰山发育有较多呈带状分布危岩体,严重威胁到沿线居民的生命财产安全。本文通过野外地质调查、遥感影像分析和数值模拟分析等方法,总结了凤凰山危岩体的崩塌失稳机理,利用动力学软件DAN-W模拟了危岩体崩塌碎屑流运动全过程,并探讨了群塌效应下碎屑流动力特征和碎屑流运动对建筑物的影响。结果表明:危岩体崩塌碎屑流动力学过程主要分为崩塌启动-碎屑流通-碎屑堆积三个阶段,危岩体BW61和BW68崩塌所产生碎屑流的最大速度分别为22.14 m/s和18.12 m/s,运动距离分别为171 m和182 m,平均厚度分别为1.57 m和1.20 m。两处危岩体发生群崩并转化为碎屑流所产生冲击压强高达132.22kPa,下方道路和居民建筑有被完全摧毁的风险。相关研究可为三峡库区危岩体风险评价和科学防控提供一定的理论依据。
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出版历程
收稿日期:  2023-05-28
修回日期:  2023-07-26

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