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青藏高原高位远程滑坡动力学研究的新问题

高浩源 高杨 殷跃平 张田田 万佳威

高浩源, 高杨, 殷跃平, 等, 2022. 青藏高原高位远程滑坡动力学研究的新问题. 地质力学学报, 28 (6): 1090-1103. DOI: 10.12090/j.issn.1006-6616.20222831
引用本文: 高浩源, 高杨, 殷跃平, 等, 2022. 青藏高原高位远程滑坡动力学研究的新问题. 地质力学学报, 28 (6): 1090-1103. DOI: 10.12090/j.issn.1006-6616.20222831
GAO Haoyuan, GAO Yang, YIN Yueping, et al., 2022. New scientific issues in the study of high-elevation and long-runout landslide dynamics in the Qinghai-Tibet Plateau. Journal of Geomechanics, 28 (6): 1090-1103. DOI: 10.12090/j.issn.1006-6616.20222831
Citation: GAO Haoyuan, GAO Yang, YIN Yueping, et al., 2022. New scientific issues in the study of high-elevation and long-runout landslide dynamics in the Qinghai-Tibet Plateau. Journal of Geomechanics, 28 (6): 1090-1103. DOI: 10.12090/j.issn.1006-6616.20222831

青藏高原高位远程滑坡动力学研究的新问题

doi: 10.12090/j.issn.1006-6616.20222831
基金项目: 

国家自然科学基金面上基金项目 42177172

国家自然科学基金青年基金项目 41907257

中国地质调查局地质调查项目 DD20221816

详细信息
    作者简介:

    高浩源(1995—), 男, 在读博士, 主要从事高位地质灾害动力成灾机理研究。E-mail: 952513795@qq.com

    通讯作者:

    高杨(1989—), 男, 副研究员, 主要从事高位地质灾害动力成灾机理研究。E-mail: 737263992@qq.com

  • 中图分类号: P642.22

New scientific issues in the study of high-elevation and long-runout landslide dynamics in the Qinghai-Tibet Plateau

Funds: 

the National Natural Science Foundation of China 42177172

the Project of the National Natural Science Foundation of China for Young Scholars 41907257

Geological Survey Project of the China Geological Survey DD20221816

  • 摘要:

    高位远程滑坡动力学机理的研究一直是国际地质灾害领域的难点问题。在青藏高原, 由于地质条件复杂, 高位远程滑坡表现出更为复杂且强烈的动力作用, 出现超高位超远程的链式成灾模式。文章针对青藏高原高位远程滑坡所表现出的三种突出动力学效应——动力破碎效应、动力侵蚀效应以及流态化效应, 从地质特征调查、物理模型试验、数值分析三个层面进行了系统性的综述。针对青藏高原高位远程滑坡目前的研究现状提出了下一步要解决的三个关键科学问题: 极端地质环境下高位远程滑坡机理研究、基于尺寸效应的模型试验新方法研究和高位远程滑坡流域性灾害链研究。这些问题将为高位远程滑坡动力学机理的研究和服务工程建设中高位远程滑坡灾害的防灾减灾提供科学依据。

     

  • 图  1  青藏高原高位远程滑坡

    a—易贡高位远程滑坡;b—色东普高位远程滑坡;c—则隆弄高位远程滑坡

    Figure  1.  High-elevation and long-runout landslides in the Qinghai-Tibet Plateau

    (a)The Yigong high-elevation and long-runout landslide; (b) The Sedongpu high-elevation and long-runout landslide; (c) The Zelongnong high-elevation and long-runout landslide

    图  2  高位远程滑坡动力作用概化图

    Figure  2.  Generalized diagram showing the dynamic action of a high-elevation and long-runout landslide

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