A semi-analytical solution for one-dimensional transient response of single-layer unsaturated porous media
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A semi-analytical solution for one-dimensional transient response of single-layer unsaturated porous media
Vol. 35, Issue 1, (2014)
作者机构:
1. 浙江大学 软弱土与环境土工教育部重点实验室,杭州,310058
2. 浙江大学 岩土工程研究所,杭州,310058
3. 中国地震局工程力学研究所,哈尔滨,150080
作者简介:
基金信息:
DOI:
CLC:TU435
Online First:14 January 2014,
Published:2014
稿件说明:
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LING Dao-sheng, WANG Yun, 2, et al. A semi-analytical solution for one-dimensional transient response of single-layer unsaturated porous media[J]. 2014, 35(1).
DOI:
LING Dao-sheng, WANG Yun, 2, et al. A semi-analytical solution for one-dimensional transient response of single-layer unsaturated porous media[J]. 2014, 35(1).DOI:
A semi-analytical solution for one-dimensional transient response of single-layer unsaturated porous media
Based on the theory of unsaturated porous media proposed by Zienkiewicz
considering the inertia
viscous and mechanical couplings and the compressibility of fluid and solid particles
semi-analytical solutions for one-dimensional transient response of single-layer unsaturated porous media are obtained with the example of a typical boundary condition problem. During the solution procedure
the dimensionless displacement governing equations in matrix form are derived firstly. Then the the nonhomogeneous boundary conditions are transformed into homogeneous boundary conditions and the eigenvalue problems of the governing equations are solved. After that
the variation coefficient method and the orthogonality of the characteristics functions are utilized to obtain a series of ordinary differential equations with their initial conditions. Applying the precise time-integration method
the semi-analytical solutions of the ordinary differential equations are developed. Finally
several numerical examples are provided to prove the correctness of the present solution and investigate the features of one-dimensional transient response of unsaturated single-layer porous media. This method can be extended to any other boundary conditions.