3-D Dynamic Response of Transversely Isotropic Saturated Soils

WANG Xiao-gang; HUANG Yi

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WANG Xiao-gang, HUANG Yi. 3-D Dynamic Response of Transversely Isotropic Saturated Soils[J]. Applied Mathematics and Mechanics, 2005, 26(11): 1278-1286.

Citation:

WANG Xiao-gang, HUANG Yi. 3-D Dynamic Response of Transversely Isotropic Saturated Soils[J]. Applied Mathematics and Mechanics, 2005, 26(11): 1278-1286.

Citation:

WANG Xiao-gang, HUANG Yi. 3-D Dynamic Response of Transversely Isotropic Saturated Soils[J]. Applied Mathematics and Mechanics, 2005, 26(11): 1278-1286.

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3-D Dynamic Response of Transversely Isotropic Saturated Soils

WANG Xiao-gang¹,
HUANG Yi²

1.
Department of Mechanical and Electrical Engineering & Architecture, Taizhou University, Linhai, Zhejiang 317000, P. R. China;

Received Date: 2004-10-10
Rev Recd Date: 2005-05-31
Publish Date: 2005-11-15

Abstract

Abstract

A study on dynamic response of transversely isotropic saturated poroelastic media under a circular non-axisymmetica harmonic source has been presented by HUANG Yi et al.using the technique of Fourier expansion and Hankel transform.However,the method may not always be valid.The work is extended to the general case being in the rectangular coordinate.The purpose is to study the 3-d dynamic response of transversely isotropic saturated soils under a general source distributing in arbitrary rectangular zoon on the medium surface.Based on Biot's theory for fluid-saturated porous media,the 3-d wave motion equations in rectangular coordinate for transversely isotropic saturated poroelastic media were transformed into the two uncoupling governing differential equations of 6-order and 2-order respectively by means of the displacement functions.Then,using the technique of double Fourier transform,the governing differential equations were easily solved.Integral solutions of soil skeleton displacements and pore pressure as well as the total stresses for poroelastic media were obtained.Furthermore,a systematic study on half-space problem in saturated soils was performed.Integral solutions for surface displacements under the general harmonic source distributing on arbitrary surface zone,considering both case of drained surface and undrained surface,were presented.
- Biot’s wave equation,
- transversely isotropic saturated poroelastic medium,
- half-space,
- harmonic response

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References(11)

References

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