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饶平平,李镜培,詹 乐.邻近斜坡沉桩挤土效应颗粒流数值模拟水资源与水工程学报[J].,2013,24(4):1-5
邻近斜坡沉桩挤土效应颗粒流数值模拟
Numerical simulation of particle flow code(PFC) of soil squeezing effect by pile sinking adjacent to slope
投稿时间:2013-01-16  
DOI:
中文关键词:  邻近斜坡  沉桩  挤土效应  颗粒流
英文关键词:adjacent to slope  sinking pile  soil squeezing effect  particle flow code
基金项目:国家自然科学基金青年基金(51208301); 国家自然科学基金项目(41272288); 上海高校青年教师培养资助计划项目(slg12019) 
作者单位
饶平平 上海理工大学 环境与建筑学院, 上海 200093 
李镜培 同济大学 地下建筑与工程系, 上海 200092 
詹 乐 同济大学 地下建筑与工程系, 上海 200092 
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中文摘要:
      邻近斜坡沉桩问题近年来在工程实践中经常遇到,由此引发的工程事故时有发生。由于沉桩边界条件的非轴对称特性,理论分析方法精确求解会遇到较多困难。本文采用离散单元法二维颗粒流程序(PFC2D),克服传统的连续介质力学模型的宏观连续性假设,研究沉桩过程中斜坡土体的挤土位移场变化规律。结果表明:随着桩体的不断沉入,斜坡挤土位移影响范围越来越大,斜坡土体的位移模式也不断发生变化;紧邻桩身以及靠近桩端范围内的土体,在桩体径向挤压以及桩侧摩擦的共同作用下,产生了向下的位移,而桩身一定距离以外的土体,受地表及倾斜自由边界的影响,表现为竖向隆起位移;当沉桩至斜坡底面以下深度时,后续沉桩对斜坡的挤土位移影响不大。
英文摘要:
      In recently years, the problem of pile sinking adjacent to slope often happen in the practice and initiates many engineering accidents. Due to the non-axisymmetric characteristics of pile sinking boundary conditions, it is difficult to solve this problem by theoretical solution. The paper used the two-dimensional particle flow code (PFC2D) of discrete element method to analyze the slope squeezing displacement under pile sinking adjacent to slope in the process of pile sinking, which can overcome the macroscopic continuity hypothesis of traditional continuum mechanics model. The results show that the influence scope of slope squeezing displacement is more and more larger with the constantly pile sinking, and the squeezing displacement mode of slope also gradually changes; soil adjacent to the pile body and pile terminals produces downward displacement under the combined action of radial extrusion of pile and its side friction, the squeezing displacement of the soil in a certain distance away from the pile body produces vertical uplift displacements under the influence of soil surface and inclined free boundary; the subsequent pile sinking has little influences on slope squeezing displacement when the pile sink to the area below the slope bottom.
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