岩土力学 ›› 2020, Vol. 41 ›› Issue (10): 3456-3464.doi: 10.16285/j.rsm.2020.0058

• 数值分析 • 上一篇    下一篇

陡倾软硬互层顺向坡强震裂隙发育特征及 边际谱熵值响应规律

李龙起,何川,王滔,赵瑞志,巨能攀   

  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,四川 成都 610059
  • 收稿日期:2020-01-17 修回日期:2020-06-11 出版日期:2020-10-12 发布日期:2020-11-07
  • 作者简介:李龙起,男,1986年生,博士,副教授,硕士生导师,主要从事地质工程和岩土工程的教学和科研工作。
  • 基金资助:
    国家自然科学基金(No. 41502299);四川省科技厅基础研究(No. 2019YJ0499);地质灾害防治与地质环境保护国家重点实验室自主研究课题(No. SKLGP2016Z007,No. SKLGP2018Z017)。

Study on fracture development characteristics and marginal spectral entropy response of soft and hard interbedded slope with steep inclination subjected to strong earthquakes

LI Long-qi, HE Chuan, WANG Tao, ZHAO Rui-zhi, JU Neng-pan   

  1. State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, Sichuan 610059, China
  • Received:2020-01-17 Revised:2020-06-11 Online:2020-10-12 Published:2020-11-07
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (41502299), the Fundamental Research of Sichuan Department of Science and Technology (2019YJ0499) and the State Key Laboratory of Geohazard Prevention and Geoenvironment Protection Independent Research Project (SKLGP2016Z007, SKLGP2018Z017).

摘要: 为揭示陡倾软硬互层顺向坡强震变形破坏过程中加速度响应与损伤裂隙扩展之间的关系,在前期离心机振动台试验的基础上,采用通用离散元(UDEC)Voronoi节理划分方法再现斜坡变形破坏过程。并基于Fish语言编程动态追踪不同振幅作用下坡体内部拉张、剪切裂隙分布情况,进而借助边际谱熵值概念建立裂隙演化与力学响应之间的关系。结果表明:(1)陡倾软硬互层坡体变形破坏过程为顶部拉裂、坡体下座?坡脚锁固段剪断、整体破坏;(2)在水平振动荷载作用初期,坡体内部裂隙发育主要受拉张作用影响,随振幅增加,裂隙扩展主要由拉张和剪切作用共同引起;(3)坡体内部各监测点边际谱熵值变化与相应位置损伤发育程度密切相关,坡内损伤较小时,边际谱熵值增加,但当坡内出现较大损伤时,边际谱熵值反而降低;(4)基于各监测点边际谱熵值变化可界定坡体变形破坏过程及滑面深度。

关键词: 软硬互层边坡, UDEC, Voronoi, 裂隙分布, 边际谱熵

Abstract: To reveal the relationship between the acceleration response and the fracture expansion of the soft and hard interbedded steep slope due to strong seismic deformation action, centrifuge table tests were conducted and the Voronoi joint division method in universal distinct element code (UDEC) was used to replicate the deformation and failure process. The tension and shear fracture distributions in the slope affected by different amplitudes were traced based on Fish programming, and then the relationship between the fracture evolution and mechanical response was established on the basis of the marginal spectral entropy concept. The results show that: 1) The deformation and failure process of the soft and hard interbedded slope with steep inclination is as follows: top tension crack, bottom-slope-foot shear and whole failure. 2) At the initial stage of horizontal vibration load, the crack development is mainly affected by the tension, and with the increase in amplitude, the crack expansion is mainly caused by the combined tension and shear actions. 3) The variation of the marginal spectral entropy of the monitoring points in the slope body is closely related to the damage degree of the corresponding position. The marginal spectral entropy value increases when the damage of the slope is slight, whereas the marginal spectral entropy decreases with severer damage of the slope. 4) The deformation failure process of the slope body and the depth of the sliding surface can be determined based on the variation in the marginal spectral entropy value of each monitoring point.

Key words: soft and hard interbedded rock slope, UDEC, Voronoi, fracture distribution, marginal spectral entropy

中图分类号: P 65
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