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Response Spectral Amplification Ratios From 1- And 2-dimensional Nonlinear Soil Site Models

机译:一维和二维非线性土壤场地模型的响应谱放大率

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In order to determine the effect of geometry on the ground response of 2-dimensional (2-D) basins filled with soils that can develop nonlinear response, we use three basin models with width/depth ratios 3, 6 and 10. The three basins are subjected to a suite of rock site records with various magnitudes and source distances. We compute response spectral amplification ratios at four locations on the surface of the 2-D basins, and determine the average variation of the amplification ratios with respect to excitation spectra, for peak ground acceleration (PGA) and 3 spectral periods of 0.2, 0.5,1 s. Similarly, we compute the average response spectral amplification ratios for two 1-dimensional (1-D) nonlinear models, one having the soil profile at the basin centre and the other having a soil profile at half the depth of the basin. From the relationship between the average amplification ratios and excitation spectra, we determine the cross-over point in terms of excitation spectral values that separate the amplification range from the deamplification range. Our results show that the cross-over point varies significantly from one location to another on the ground surface and from one basin to another, in a range of 0.3-1.lg for PGA. The effects of basin geometry are very strong at weak and moderate excitation, but decrease with increasing excitation spectra in a significant portion around the basin centre. Our results provide some justification for using 1-D models for 2-D basins with a width/depth ratio ≥6 if the soil site is subjected to strong ground shaking.
机译:为了确定几何形状对填充有可发展非线性响应的土壤的二维(2-D)盆地地面响应的影响,我们使用宽度/深度比为3、6和10的三个盆地模型。这三个盆地受到一系列不同大小和震源距离的岩石现场记录的影响。我们计算了二维盆地表面上四个位置的响应光谱放大率,并确定了对于峰值地面加速度(PGA)和3个光谱周期为0.2、0.5, 1秒同样,我们为两个一维(1-D)非线性模型计算平均响应光谱放大率,其中一个模型在盆地中心具有土壤剖面,另一个模型在盆地深度的一半处具有土壤剖面。根据平均放大率与激发光谱之间的关系,我们根据将放大范围与去放大范围分开的激发光谱值来确定交叉点。我们的结果表明,在地面上,从一个位置到另一个位置,从一个盆到另一个盆,交叉点的变化很大,对于PGA,范围在0.3-1.lg之间。在弱和中度激发下,盆地几何形状的影响非常强烈,但在盆地中心附近的很大一部分,随着激发光谱的增加而减小。如果土壤位置受到强烈的地面震动,我们的结果为将一维模型用于宽度/深度比≥6的二维盆地提供了一些依据。

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