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ANALYTICAL SOLUTIONS OF THE SCATTERING OF PLANE WAVES BY LOCAL SITES WITH SATURATED SOIL

机译:饱和土体局部平面波散射的解析解

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The ground amplification effects caused by irregular surface topography and geological conditions have been the focus of research by both seismologists and earthquake engineers for the last three decades. Many methods have been developed. However, only few analytical solutions are available so far, and the majority of the solutions for the wave propagation are supposed in the single-phase elastic medium. In this paper, the earthquake ground motions of local irregular sites with saturated soil were investigated by analytical solutions, and a series of results were obtained. Firstly, on the basis of Biot dynamic theory, an analytical method for scattering of plane waves by saturated soil was developed using Fourier-Bessel series expansion technique.Using this method, a series of analytical solutions for scattering of plane waves by saturated soil local irregular site can be got. Secondly, on the base of the analytical solutions mentioned above, the numerical results were given to illustrate that the ground motions of the saturated soil local irregular site not only depend on the angle of incidence, the dimensionless frequency of the incident waves, but also depend on the saturation and porosity of the soil deposits, the stiffness and Poisson?s ratio of the solid-skeleton, and the boundary conditions. At the same time,the soft saturated soil site can be simulated by elastic one-phase solid model or by fluid-saturated porous media model, but the results of the ground motion by the two models were great different.
机译:在过去的三十年中,由不规则的表面地形和地质条件引起的地面放大效应一直是地震学家和地震工程师的研究重点。已经开发了许多方法。但是,到目前为止,只有很少的解析解可用,并且大多数用于波传播的解都假设在单相弹性介质中。本文通过解析解研究了局部不饱和场地饱和土的地震地震动,获得了一系列结果。首先,基于Biot动力学理论,提出了一种利用傅立叶-贝塞尔级数展开技术对饱和土散射平面波的解析方法,并利用该方法提出了一系列对饱和土局部不规则平面波散射的解析解。网站可以得到。其次,在上述解析解的基础上,给出了数值结果,说明了饱和土局部不规则部位的地震动不仅取决于入射角,入射波的无量纲频率,还取决于沉积物的饱和度和孔隙率,固体骨架的刚度和泊松比以及边界条件。同时,可以通过弹性的一相固体模型或流体饱和的多孔介质模型来模拟软饱和土场地,但两种模型的地震动结果却大不相同。

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