长江科学院院报 ›› 2016, Vol. 33 ›› Issue (5): 111-115.DOI: 10.11988/ckyyb.20150140

• 岩土工程 • 上一篇    下一篇

类土质边坡失稳机理分析与稳定性研究

李满意1,2, 周洪燕3, 魏燕珍1, 史玲1   

  1. 1.重庆市地质灾害自动化监测工程技术研究中心, 重庆 400042;
    2.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;
    3.重庆邮电大学移通学院 管理工程系,重庆 401520
  • 收稿日期:2015-02-25 出版日期:2016-05-01 发布日期:2016-05-10
  • 作者简介:李满意(1986-),男,安徽砀山人,工程师,硕士,主要从事岩土体稳定性评价及地质灾害防治等方面的生产及研究工作,(电话)15213097163 (电子信箱)562365608@qq.com。

Instability Mechanism and Stability Analysis of Soil-like Slope

LI Man-yi1,2, ZHOU Hong-yan3, WEI Yan-zhen1, SHI Ling1   

  1. 1.Chongqing Engineering Research Center of Automatic Monitoring for Geological Hazards, Chongqing 400042, China;
    2.State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology, Chengdu 610059, China;
    3. Management Engineering, College of Mobile Telecommunications, Chongqing University of Posts and Telecommunications, Chongqing 401520, China
  • Received:2015-02-25 Online:2016-05-01 Published:2016-05-10

摘要: 类土质边坡工程特性及稳定性明显区别于一般的均质土边坡和岩质边坡,实际生产项目中,工程技术人员多将其视为一般的均质土边坡进行勘察、设计,造成了设计浪费或设计失败,因此对类土质边坡变形的地质力学模式及失稳机理的研究具有实用价值。以重庆市合川区狮滩镇洞堂湾边坡为地质原型,在对边坡赋存的地质环境条件、边坡的坡体结构特征、变形破裂特征分析的基础上,得出该类边坡变形的地质力学模型为渐进后退式蠕滑-拉裂;边坡失稳机理分析结果表明该边坡多发生在暴雨或持续降雨期间,有一定的滞后特征,边坡失稳多受坡体中倾外的缓倾结构面及陡倾的裂隙面控制。最后采用平面滑动法对该边坡进行稳定性分析和评价,计算结果与边坡的变形破裂特征基本相互吻合。

关键词: 类土质边坡, 洞堂湾边坡, 地质力学模式, 失稳机理, 稳定性评价, 重庆合川区

Abstract: The engineering properties and stability of soil-like slope obviously differ from those of homogeneous soil slope and rock slope. In actual construction projects, soil-like slopes are regarded as general homogeneous soil slope and rock slope, resulting in inadequate reliability, or conservative support. Research on the geomechanical model and instability mechanism of soil-like slope is of practical significance. In this paper, Dongtangwan slope in Hechuan district of Chongqing is taken as a geological prototype to analyze the geological conditions, structural features, and deformation behaviors of the slope. Results reveal that the geomechanical model is progressive backwards creep slide-tension fracture; instability analysis shows that the failure of soil-like slope usually happens in storm or continuous rainfall, with some lag in time, and the instability is mainly controlled by the gently-inclined structural planes and steep-inclined fissure planes. Furthermore, the slope stability is analyzed and evaluated based on plane sliding mode. The calculation results are consistent with the deformation characteristics of the slope.

Key words: soil-like slope, Dongtangwan slope, geomechanical model, instability mechanism, stability assessment, Hechuan district of Chongqing

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