分析土壤半无限域的一种有限层方法(Ⅰ)——一般理论
Finite Layer Analysis for Semi-Infinite Soils (Ⅰ)——General Theory
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摘要: 本文研究了一种用于横观各向同性体动力学的有限层法.将土壤介质半无限域视为一个横观各向同性半空间体,介质的材料函数沿深度变化,将介质沿深度方向分成若干层,在每一层内材料函数用一个指数函数来模拟.这样,使求解问题的方程得到简化,利用Fourier变换我们得到了各层处“节点”力与位移的关系.这种有限层法实际上是一种半解析法.具有一般半解析法所具备的数据前后处理量少及计算量小等优点.本文所研究的这种有限层法为分析土壤与结构相互作用问题提供了一条新途径.Abstract: In the present paper a finite layer method is studied for the flastodynarnics of transverse isotropic bodies.With this method,semi-infinite soils can be considered as an transverse isotropic half-space,its material functions varying with depth.Dividing the half-space into a scries of layers in the direction of depth,the material junctions in each layer are simulated by exponential functions Consequently,the fundamental equations to be solved can be simplified if the Fourier transform with repsect to coordinates is used.We have obtained the relationship between the "layer forces" and "layer displacements".This finite layer method,in fact,can also be called a semi-analytical method.It possesses those advantages as the usual semi-analytical methods do,and can be used to analyse the problem of the interaction between soils and structures.
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Key words:
- finite layer method /
- transverse isotropy /
- semi-infinite region /
- elastodynamics
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