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A new method for solving Biot's consolidation of a finite soil layer in the cylindrical coordinate system
基金项目:The project supported by the National Natural Science Foundation of China (50578121).
摘    要:
A new method is developed to solve Biot's consolidation of a finite soil layer in the cylindrical coordinate system. Based on the governing equations of Biot's consolidation and the technique of Laplace transform, Fourier expansions and Hankel transform with respect to time t, coordinate θ and coordinate r, respectively, a relationship of displacements, stresses, excess pore water pressure and flux is established between the ground surface (z = 0) and an arbitrary depth z in the Laplace and Hankel transform domain. By referring to proper boundary conditions of the finite soil layer, the solutions for displacements, stresses, excess pore water pressure and flux of any point in the transform domain can be obtained. The actual solutions in the physical domain can be acquired by inverting the Laplace and the Hankel transforms.

关 键 词:毕奥固结  有限土壤层  拉普拉斯转换  傅里叶扩展  Hankel转换

A new method for solving Biot's consolidation of a finite soil layer in the cylindrical coordinate system
Zhiyong Ai,Quansheng Wang,Chao Wu. A new method for solving Biot's consolidation of a finite soil layer in the cylindrical coordinate system[J]. Acta Mechanica Sinica, 2008, 24(6): 691-697. DOI: 10.1007/s10409-008-0187-5
Authors:Zhiyong Ai  Quansheng Wang  Chao Wu
Affiliation:(1) Department of Geotechnical Engineering, Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University, 200092 Shanghai, China
Abstract:
A new method is developed to solve Biot’s consolidation of a finite soil layer in the cylindrical coordinate system. Based on the governing equations of Biot’s consolidation and the technique of Laplace transform, Fourier expansions and Hankel transform with respect to time t, coordinate θ and coordinate r, respectively, a relationship of displacements, stresses, excess pore water pressure and flux is established between the ground surface (z = 0) and an arbitrary depth z in the Laplace and Hankel transform domain. By referring to proper boundary conditions of the finite soil layer, the solutions for displacements, stresses, excess pore water pressure and flux of any point in the transform domain can be obtained. The actual solutions in the physical domain can be acquired by inverting the Laplace and the Hankel transforms. The project supported by the National Natural Science Foundation of China (50578121).
Keywords:Biot’  s consolidation  A finite soil layer  Laplace transform  Fourier expansions  Hankel transform
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