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3-D DYNAMIC RESPONSE OF TRANSVERSELY ISOTROPIC SATURATED SOILS
作者姓名:王小岗  黄义
作者单位:[1]Department of Mechanical and Electrical Engineering &'Architecture, Taizhou University, Linhai 317000, Zhejiang Province, -P. R. China [2]Science College, Xi' an University of Architecture & Technology, Xi'an 710055, P. R. China
基金项目:Project supported by the National Natural Science Foundation of China ( No. 56978003 ) and the Ministry of Education "Chunhui Project" Foundation of China ( No. 200309)
摘    要:Introduction Thedynamicanalysisofsaturatedporoelasticmediaisofbroadmeaninginmanyaspectssuchasseismology,earthquakeengineering,soilmechanicsandgeophysics,etc.Thetransverselyisotropicsaturatedsoilsissolid fluidcoupledtwophasemediainwhichthe soilskeletondisp…

关 键 词:Biot’s  wave  equation  transversely  isotropic  saturated  poroelastic  medium  half-space  harmonic  response  double  Fourier  transform  
文章编号:0253-4827(2005)11-1409-11
收稿时间:2004-10-10
修稿时间:2005-05-31

3-D dynamic response of transversely isotropic saturated soils
Xiao-gang Wang,Yi Huang.3-D DYNAMIC RESPONSE OF TRANSVERSELY ISOTROPIC SATURATED SOILS[J].Applied Mathematics and Mechanics(English Edition),2005,26(11):1409-1419.
Authors:Xiao-gang Wang  Yi Huang
Institution:1. Department of Mechanical and Electrical Engineering & Architecture, Taizhou University, Linhai, 317000, Zhejiang Province, P. R. China
2. Science College, Xi’an University of Architecture & Technology, Xi’an, 710055, P.R.China
Abstract:A study on dynamic response of transversely isotropic saturated poroelastic media under a circular non-axisymmetrical 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.
Keywords:Biot's wave equation  transversely isotropic saturated poroelastic medium  half-space  harmonic response  double Fourier transform
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