长江科学院院报 ›› 2017, Vol. 34 ›› Issue (10): 107-113.DOI: 10.11988/ckyyb.20160619

• 岩土工程 • 上一篇    下一篇

土质边坡归一化变形量失稳判据研究

张坤勇1a,1b,杜伟1a,1b,李广山1a,1b,钟思成2,刘子剑3   

  1. 1.河海大学 a.岩土力学与堤坝工程教育部重点实验室;b.江苏省岩土工程技术工程研究中心,南京 210098;
    2.中铁第一勘察设计院集团有限公司,西安 710043;
    3.中国公路工程咨询集团有限公司,北京 100097
  • 收稿日期:2016-06-16 修回日期:2016-07-27 出版日期:2017-10-01 发布日期:2017-10-25
  • 通讯作者: 杜 伟(1975-),男,安徽合肥人,助理工程师,硕士,研究方向为边坡稳定性分析,(电话)15295522135(电子信箱)dw1991hhu@163.com。
  • 作者简介:张坤勇(1975-),男,安徽濉溪人,副教授,硕士生导师,研究方向为土的基本特性、复杂应力状态下桩土相互作用关系以及边坡稳定安全分析,(电话)13814536929(电子信箱)ky_zhang@hhu.edu.cn。
  • 基金资助:
    国家自然科学基金项目(41530637,51578214);中央高校基本科研业务费专项资金项目(2015B17714);中国交通建设股份有限公司科技研发项目(2012-ZJKJ-11)

Normalized Failure Criterion for Soil Slope Stability

ZHANG Kun-yong1,2, DU Wei1,2, LI Guang-shan1,2, ZHONG Si-cheng3, LIU Zi-jian4   

  1. 1.Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University,Nanjing 210098, China;
    2.Jiangsu Provincial Research Center for Geotechnical Engineering Technology, Hohai University, Nanjing 210098, China;
    3.China Railway First Survey and Design Institute Group Ltd.,Xi’an 710043, China;
    4. China Highway Engineering Consulting Corporation, Beijing 100097, China
  • Received:2016-06-16 Revised:2016-07-27 Online:2017-10-01 Published:2017-10-25

摘要: 为建立土质边坡失稳的微观机理和宏观位移之间的关系,应用有限元强度折减法,分析了失稳过程中土质边坡土体单元应力状态和整体稳定性的联系,定义了边坡渐进破坏时潜在滑动面上土体单元的应力差;分别采用塑性应变区贯通、特征点位移突变、应力差等不同失稳判据对均质土坡的稳定性进行判断分析,验证了不同边坡失稳判据间的一致性与统一性。通过单因素敏感性分析方法,分析了边坡几何参数(坡高、坡比)与物理力学参数(弹性模量、重度、黏聚力、内摩擦角和泊松比等)对极限状态下边坡坡顶水平位移的影响;结合归一化变量的变异系数法,构建了以变形量为基础,同时考虑几何因素与物理因素的土质边坡归一化失稳判据,提出了边坡稳定性的评价方法。

关键词: 土质边坡, 归一化变形量, 失稳判据, 强度折减有限元法, 整体稳定性

Abstract: In the aim of obtaining the relationship between microcosmic mechanism of soil slope instability and macroscopic displacement, a method of slope stability evaluation is proposed. The internal correlation between the soil element stress and the whole stability in the process of soil slope sliding was analyzed through shear strength reduction finite element method, and the stress difference of soil unit on the potential sliding surface during progressive failure of slope was defined. In subsequence, the consistency and uniformity among different criteria, including plastic zone penetration, abrupt change of characteristic displacement, and stress difference, were verified through instability evaluation. Furthermore, the influences of geometric and physical parameters on the horizontal displacement of slope top in limit state were analyzed through single-factor sensitivity analysis method. These parameters include slope height, slope ratio, elastic modulus, density, cohesion, internal friction angle, and Poisson ratio. Finally, the normalized failure criterion for soil slope based on deformation in consideration of both geometric and physical factors was established through the method of coefficient of variation.

Key words: soil slope, normalized variables, failure criterion, shear strength reduction FEM, global stability

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