横观各向同性饱和地基上无限板的稳态振动

研究了横观各向同性饱和土地基上无限板的稳态振动问题. 基于直角坐标系下横观各向同性饱和介质Biot波动方程的一般解，采用双重Fourier积分变换技术，建立了饱和地基与无限矩形板相互作用的动力方程，利用数值方法求解该方程，得到任意谐振荷载作用下饱和半空间体上无限板稳态响应的一般解. 数值结果表明，横观各向同性饱和地基上无限板的振动与各向同性饱和地基上的无限板的振动特性存在明显差异.     

横观各向同性饱和介质非轴对称动力响应分离变量解Separation of variables solution of non-axisymmetrical dynamic response of transversely isotropic saturated porous media

首先将横观各向同性饱和弹性多孔介质非轴对称问题的Bio t波动方程,变换为适宜于进行分离变量法求解的形式;然后在非轴对称简谐激励下,用分离变量法得到Bio t方程的一般解,即用分离变量法求得了多孔介质位移和应力分量的解析表达式;并给出了半空间横观各向同性饱和弹性多孔介质在表面竖向简谐荷载作用下表面竖向位移的数值分析结果,得出载荷对30倍受载半径以外的区域几乎无影响的结论。同时表明了本文的分析方法是切实可行的。     

横观各向同性饱和介质非轴对称动力响应分离变量解

首先将横观各向同性饱和弹性多孔介质非轴对称问题的Biot波动方程,变换为适宜于进行分离变量法求解的形式;然后在非轴对称简谐激励下,用分离变量法得到Biot方程的一般解,即用分离变量法求得了多孔介质位移和应力分量的解析表达式;并给出了半空间横观各向同性饱和弹性多孔介质在表面竖向简谐荷载作用下表面竖向位移的数值分析结果,得出载荷对30倍受载半径以外的区域几乎无影响的结论。同时表明了本文的分析方法是切实可行的。     

横观各向同性饱和地基上中厚圆板的非轴对称振动

研究横观各向同性饱和土地基上中厚弹性圆板的非轴对称振动问题。基于横观各向同性饱和介质Biot波动方程的一般解,按混合边值问题建立了饱和地基与弹性中厚圆板非轴对称动力相互作用的对偶积分方程,并将对偶积分方程转化为易于计算的第二类Fredholm积分方程;采用数值方法求解该积分方程。数值算例结果表明,当h/a>0.05时,饱和半空间体上中厚度圆板在不同频率下的振动特性与相应频率下的刚性板的振动特性基本相同,当h/a<0.05时,板中心的位移将随h/a的减小而增大。     

横观各向同性饱和土中柱面载荷的动力Green函数

基于饱和介质的三维波动理论的Biot模型,利用Fourier展开和Hankel变换,并借助算子理论,给出了圆柱坐标系下横观各向同性饱和土波动方程的非轴对称通解;利用通解,建立了饱和土层及饱和半空间的精确动力刚度矩阵;借助刚度矩阵,给出层状横观各向同性饱和地基中,作用沿土层深度方向分布的竖向和水平柱面载荷时的动力Green函数,进而解决了利用间接边界元法分析桩-饱和土动力相互作用的关键问题.     

层状横观各向同性饱和土的非轴对称动力响应

通过方位角的Fourier变换，将圆柱坐标系下横观各向同性饱和土的Biot非轴对称波动方 程转化为一组一阶常微分方程组. 然后基于径向Hankel变换,建立问题的状态方程；求解状态方程后,得到传递矩阵. 进而利用传递矩阵，结合饱和层状地基的边界条件、排水条件及层间接触和连续条件,求解 了任意震源力作用下层状横观各向同性饱和地基频域动力响应问题. 时域解可通过频率的Fourier积分得到.     

横观各向同性饱和多孔半平面与梁的动力相互作用

以Biot理论为基础,通过引入一个函数Φ,将横观各向同性饱和多孔半平面的基本方程组简化为一个6阶控制方程.利用Fourier变换,分析了横观各向同性饱和多孔半平面体的动力响应.利用Fourier变换或正弦级数,研究了该介质上梁的简谐振动问题,将原先极为复杂的问题转化为数值积分问题.文末还对横观各向同性饱和多孔半平面与梁的相互作用问题进行了数值计算.     

横观各向同性饱和多孔半空间与梁的动力相互作用

通过引入三个标量函数,结合Fourier变换,首先将横观各向同性饱和多孔半空间的基本方程组简化为一个6阶控制方程和一个2阶控制方程;求解这两个控制方程,给出了横观各向同性饱和多孔半空间相关物理量的解析表达式.利用带扩展项的正弦级数解答,在将梁下地基表面沉降也展成正弦级数后,结合板-地基的相容条件(连续条件),对横观各向同性饱和多孔半空间与有限长梁的动力相互作用问题进行了分析、计算.另外,利用Fourier变换,对横观各向同性饱和多孔半空间与无限长梁的动力相互作用问题进行了分析.     

横观各向同性饱和层状地基的三维稳态动力响应

首先引入状态向量,将直角坐标系下横观各向同性饱和土的Biot波动方程转化为一组状态方程,然后基于双重Fourier变换,求解了状态方程,得到传递矩阵.进而利用传递矩阵,并结合饱和地基的边界条件、排水条件及层间接触和连续条件,求解了横观各向同性饱和层状地基的稳态动力响应问题.     

横观各向同性热弹性多孔介质板的精化理论

研究了孔隙水压力作用下横观各向同性热弹性多孔介质板的精化理论。在不做任何预先假设的情况下,利用Lur’e方法和横观各向同性热弹性多孔介质的通解,得到了横观各向同性热弹性多孔介质板的精化理论。首先,根据调和函数的sin算子函数表达式,得到了用5个二维待定函数表示的位移场和应力场;其次,在非齐次边界条件下,利用基本的数学算法,得到了在孔隙水压力载荷作用下热弹性多孔介质板的精化方程;最后,通过舍弃高阶项,得到了位移场和应力场的近似解。     

3-D DYNAMIC RESPONSE OF TRANSVERSELY ISOTROPIC SATURATED SOILS

Introduction Thedynamicanalysisofsaturatedporoelasticmediaisofbroadmeaninginmanyaspectssuchasseismology,earthquakeengineering,soilmechanicsandgeophysics,etc.Thetransverselyisotropicsaturatedsoilsissolid fluidcoupledtwophasemediainwhichthe soilskeletondisp…     

The Non-Axisymmetrical Dynamic Response of Transversely Isotropic Saturated Poroelastic Media

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Dynamic interaction between elastic thick circular plate and transversely isotropic saturated soil ground

IntroductionThe vibration of the plate on the porous saturated building foundation is a complicateddynamic contact problem.Its consideration is very important in both earthquake and geo-technical engineering.Lots of research works have been done in recent…     

Non-axisymmetrical vibration of elastic circular plate on layered transversely isotropic saturated ground

The non-axisymmetrical vibration of elastic circular plate resting on a layered transversely isotropic saturated ground was studied.First,the 3-d dynamic equations in cylindrical coordinate for transversely isotropic saturated soils were transformed into a group of governing differential equations with 1-order by the technique of Fourier ex- panding with respect to azimuth,and the state equation is established by Hankel integral transform method,furthermore the transfer matrixes within layered media are derived based on the solutions of the state equation.Secondly,by the transfer matrixes,the general solutions of dynamic response for layered transversely isotropic saturated ground excited by an arbitrary harmonic force were established under the boundary conditions, drainage conditions on the surface of.ground as well as the contact conditions.Thirdly, the problem was led to a pair of dual integral equations describing the mixed boundary- value problem which can be reduced to the Fredholm integral equations of the second kind solved by numerical procedure easily.At the end of this paper,a numerical result concerning vertical and radical displacements both the surface of saturated ground and plate is evaluated.     

TORSIONAL VIBRATIONS OF RIGID CIRCULAR PLATE ON TRANSVERSELY ISOTROPIC SATURATED SOIL

An analytical method was presented for the torsional vibrations of a rigid disk resting on transversely isotropic saturated soil. By Hankel transform, the dynamic governing differential equations for transversely isotropic saturated poroelastic medium were solved. Considering the mixed boundary-value conditions, the dual integral equations of torsional vibrations of a rigid circular plate resting on transversely isotropic saturated soil were established. By appropriate transform, the dual integral equations were converted into a Fredholm integral equation of the second kind. Subsequently, the dynamic compliance coefficient, the torsional angular amplitude of the foundation and the contact shear stress were expressed explicitly. Selected examples were presented to analyse the influence of saturated soil's anisotropy on the foundation's vibrations.