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平面应变Biot固结的解析层元
引用本文:艾智勇,曹国军,成怡冲.平面应变Biot固结的解析层元[J].力学学报,2012,44(2):401-407.
作者姓名:艾智勇  曹国军  成怡冲
作者单位:同济大学地下建筑与工程系, 岩土及地下工程教育部重点实验室, 上海 200092
基金项目:国家自然科学基金资助项目(50578121)~~
摘    要:提出用解析层元法有效地解决任意深度单层土的平面应变 Biot 固结问题. 从 Biot 固结问题的控制方程出发, 采用特征值法在 Laplace-Fourier 变换域内推导出一个精确对称的解析层元刚度矩阵. 通过表示单层土广义力和广义位移之间关系的解析层元, 并结合土层的边界条件, 推导出土层任意点的解答; 物理域内的真实解可以通过 Laplace-Fourier 数值逆变换进一步获得. 通过数值计算验证理论的正确性, 研究了土层性质及时间因素对固结的影响.}

关 键 词:解析层元  平面应变Biot固结  Laplace-Fourier变换  特征值法
收稿时间:2010-11-24
修稿时间:2011-06-17

ANALYTICAL LAYER-ELEMENT OF PLANE STRAIN BIOT’S CONSOLIDATION
Ai Zhiyong,Cao Guojun Cheng Yichong.ANALYTICAL LAYER-ELEMENT OF PLANE STRAIN BIOT’S CONSOLIDATION[J].chinese journal of theoretical and applied mechanics,2012,44(2):401-407.
Authors:Ai Zhiyong  Cao Guojun Cheng Yichong
Institution:Department of Geotechnical Engineering, Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University, Shanghai 200092, China
Abstract:An efficient algorithm is presented to solve plane strain Biot’s consolidation of a single soil layer with an arbitrary depth.Starting from the governing equations of Biot’s consolidation,an exactly symmetric stiffness matrix,i.e.the analytical layer-element,is deduced in Laplace-Fourier transformed domain by using the eigenvalue approach.According to the relationship between generalized displacements and stresses of a single layer in the transformed domain described by the matrix,and the boundary conditions of the soil layer, the solutions of any point can be obtained.The actual solutions in the physical domain can further be acquired by inverting the Laplace-Fourier transform.Finally,numerical examples are presented to verify the theory and study the influence of the soil properties and time history on the consolidation behavior.
Keywords:analytical layer-element  plane strain Biot’s consolidation  Laplace-Fourier transform  eigenvalue approach
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