长江科学院院报 ›› 2017, Vol. 34 ›› Issue (4): 117-121.DOI: 10.11988/ckyyb.20151048

• 岩土工程 • 上一篇    下一篇

黄河某水电站库区Ⅲ#滑坡形成机制研究

王云南,任光明,邱 俊   

  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,成都 610059
  • 收稿日期:2015-12-14 出版日期:2017-04-01 发布日期:2017-04-10
  • 作者简介:王云南(1991-),男,吉林吉林市人,硕士研究生,主要从事边坡稳定性及工程效应研究工作,(电话)18781952110(电子信箱)605725462@qq.com。
  • 基金资助:
    国家自然科学基金项目(41072229)

Formation Mechanism of Landslide in the Reservoir Area ofa Hydropower Station of the Yellow River

WANG Yun-nan, REN Guang-ming, QIU Jun   

  1. State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection,Chengdu University of Technology, Chengdu 610059, China
  • Received:2015-12-14 Online:2017-04-01 Published:2017-04-10

摘要: 倾倒-变形多发生在逆向层状边坡内,但在近几年工程勘查中发现,陡倾顺向边坡也存在该种失稳模式,研究其形成机制对正确评价工程边坡的稳定性有着重要意义。以西北黄河流域某水电站坝前右岸的Ⅲ#滑坡为例,在地质勘察的基础上,结合数值模拟和定性分析得出滑坡的形成过程分为河谷下切、坡表卸荷,岩层发生倾倒-变形,滑移-拉裂3个阶段,利用UDEC再现了滑坡的形成过程。利用有限元和离散元计算得到的结果互相吻合,证明了结论的合理性。

关键词: 滑坡, 顺向边坡, 形成机制, 倾倒-变形, 数值模拟

Abstract: Toppling-deformation is usually found in anti-dip bedded slopes. But recent engineering investigations revealed that toppling-deformation mode could also appear in steep dip bedding slope. Analyzing the formation mechanism is of importance for the correct assessment of slope stability. In this article, the landslide III# on the right bank of a hydropower station in the Yellow River Basin was researched by means of numerical simulation and qualitative analysis based on geological surveys. The process of landslide formation was displayed by UDEC (Universal Distinct Element Code). Results indicated that the failure process of the landslide could be divided into three stages rock mass unloading, toppling deformation, and sliding-tension fracture. The result obtained from finite element method consists with that from discrete element method, which proves that the conclusion is rational.

Key words: landslide, dip bedding slope, formation mechanism, toppling-deformation, numerical modeling

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