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顺层页岩边坡稳定性离散元分析
引用本文:张小勇,李晓军.顺层页岩边坡稳定性离散元分析[J].西北地震学报,2017,39(5):957-962.
作者姓名:张小勇  李晓军
作者单位:西安科技大学, 陕西 西安 710054,西安科技大学, 陕西 西安 710054
摘    要:以承张高速某顺层页岩边坡工程为依托,首先采用单轴压缩模拟实验与宏观力学参数值对比的方法确定出边坡各岩土层的细观参数。进而建立其离散元模型,分析其稳定状态,并对其失稳过程进行研究。结果表明:边坡中的全风化页岩层向下滑动,并在坡脚堆积;强风化页岩层和中风化页岩层未发生滑动,滑动面为全风化页岩层与强风化页岩层的交界面。模型中出现的裂纹主要以压裂纹为主,且主要分布在全风化层,而其他两层未产生裂纹。离散元模拟结果与赤平投影法分析结果一致。该模拟结果对工程的设计、施工具有指导意义。

关 键 词:顺层页岩边坡  单轴压缩  离散元模型
收稿时间:2016/4/25 0:00:00

Discrete Element Numerical Simulation on Stability of Bedding Shale Slope
ZHANG Xiaoyong and LI Xiaojun.Discrete Element Numerical Simulation on Stability of Bedding Shale Slope[J].Northwestern Seismological Journal,2017,39(5):957-962.
Authors:ZHANG Xiaoyong and LI Xiaojun
Institution:Xi''an University of Science and Technology, Xi''an 710054, China and Xi''an University of Science and Technology, Xi''an 710054, China
Abstract:Slope,which is a natural geological integration,can be divided into two types-soil slope and rock slope.Qualitative analysis and quantitative analysis are often used in the slope stability assessment.DEM used in this paper belongs to quantitative analysis.The traditional approaches to slope stability assessment are hardly to reflect the unstability mode and destruction process.However,DEM owns apparent advantages on the analysis of non-continuum medium''s deformation and destruction.Based on the bedding shale slope in debris deposit,the meso-parameters of PFC model was determinated by comparison of meso-parameters in simulated uniaxial compression test and macro mechanics parameters.It shows that the parameters used in the former simulations could be used in the subsequent stability assessment model of slope.Expasion method was used to establish the model in this paper.In this method,balls were generated in specified areas.Then the radius of balls were enlarged until contact forces were generated.Balls were driven to move around for balance and then the areas were filled with balls.A general study on stable state of the slope was carried out using DEM.Sliding process and sliding distance were also studied.The results show that:the completely weathered shale slipped down and deposited at the bottom of the slope.The strong weathered shale and intermediary weathered shale didn''t slip.The sliding surface was a interface between completely weathered shale and strong weathered shale.Compression fractures are the primary fractures which only occur on the completely weathered layer.Owning to the small strength of the completely weathered shale layer,most parallel bonds break because of gravity.Grains'' spilling out of the bottom makes the middle-upper grains slide downwards on account of lacking supports.Based on the analysis above,cutting slope should be adopted.The simulation results are in agreement with the stereographic method,and it can instruct the design and construction of the project.
Keywords:Bedding shale slope  uniaxial compression  discrete element model of slope
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