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RANDOM VIBRATION THEORY BASED SEISMIC SITE RESPONSE ANALYSIS

机译:基于随机振动理论的地震场地响应分析

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In this paper, an alternative approach for seismic site response analysis is presented. This approach is based on Random Vibration Theory (RVT) and works in frequency domain. With this approach, the need for time history generation is eliminated and the responses are computed at the selected confidence level. This approach follows the SHAKE theoretical framework and is based on closed form solution of one-dimensional wave propagation. The main difference with the commonly used approach in the program SHAKE are as follows:response spectrum.the response is obtained. The peak factors for the PSD responses are computed and the statistical means of the maximum responses are computed. The maximum shear strain in each soil layer is used to iterate on soil properties using the strain-dependent soil properties of each layer based on the equivalent linear method until convergence is reached for all soil layers.spectra, peak shear stress and strains are obtained.the analysis.This approach has been implemented in a new computer program named P-SHAKE and has been used successfully in recent projects. This paper provides the theoretical basis of the approach and presents a comparison of the P-SHAKE and SHAKE results and describes the advantages and limitations of the new method.
机译:在本文中,提出了一种用于地震现场响应分析的替代方法。该方法基于随机振动理论(RVT),并且在频域中工作。通过这种方法,消除了对时间历史记录的需求,并在选定的置信度水平上计算了响应。该方法遵循SHAKE理论框架,并且基于一维波传播的封闭形式解决方案。与SHAKE程序中常用方法的主要区别如下:响应频谱。计算PSD响应的峰值因子,并计算最大响应的统计平均值。基于等效线性方法,使用每一层的应变相关土壤特性,使用每个土壤层中的最大剪切应变来迭代土壤特性,直到所有土壤层都达到收敛为止,从而获得光谱,峰值剪切应力和应变。该方法已在名为P-SHAKE的新计算机程序中实现,并已成功用于最近的项目中。本文提供了该方法的理论基础,并对P-SHAKE和SHAKE结果进行了比较,并描述了该新方法的优点和局限性。

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