Soil amplification: some refinements

Eduardo Kausel, JoséM. Roësset
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引用次数: 24

Abstract

The most widely used techniques for the study of one-dimensional amplification of vertically propagating seismic waves involve solution of the dynamic equations in the frequency domain with linearly viscoelastic material properties. Material nonlinearities are approximately modeled by iterative use of linear solutions, adjusting values of modulus and damping until they are compatible with computed levels of strain. The program SHAKE is the best known example of a code using this procedure.

Several refinements to the iterative scheme originally proposed by Seed and Idriss are presented in this paper. In particular, it is shown that the solution for the layers underlying the control motion can be obtained in one single step, when the mass matrix is diagonal. Use of the shear stress in place of the shear strain as the controlling parameter in determining material properties gives faster convergence and identifies cases of potential non-convergence. Trivial modifications are also proposed to the standard scheme that would enable the researcher to study the amplification or deconvolution of non-vertically incident SH waves with a code like SHAKE. These modifications consist simply in changing the mass density of the soil, and redefining the characteristic strain.

土壤放大:一些细化
研究垂直传播地震波一维放大的最广泛的技术是求解具有线性粘弹性材料特性的频域动力学方程。材料非线性通过线性解的迭代近似建模,调整模量和阻尼的值,直到它们与计算的应变水平相容。程序SHAKE是使用此过程的最著名的代码示例。本文对Seed和Idriss提出的迭代格式进行了改进。特别是,当质量矩阵为对角线时,控制运动底层的解可以在一步中得到。使用剪切应力代替剪切应变作为确定材料性能的控制参数,可以更快地收敛并识别潜在的不收敛情况。对标准方案也提出了一些微小的修改,使研究人员能够用类似SHAKE的代码研究非垂直入射SH波的放大或反卷积。这些修改仅仅是改变土壤的质量密度,并重新定义特征应变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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