与指定地震记录相关的非平稳地震动场的模拟

杨娜 田玉基 杨庆山

振动与冲击 ›› 2012, Vol. 31 ›› Issue (19) : 36-39.

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PDF(1617 KB)
振动与冲击 ›› 2012, Vol. 31 ›› Issue (19) : 36-39.
论文

与指定地震记录相关的非平稳地震动场的模拟

  • 杨娜 田玉基 杨庆山
作者信息 +

Artificial Ground Motions Correlated to a Specified Earthquake Record

  • Na Yang, Yu,ji TIAN and Qing,shan YANG
Author information +
文章历史 +

摘要

地震动的非平稳特性主要是由其相位差谱决定的,相位差谱与相位导数之间存在线性倍数关系。根据相位导数的计算公式,从能量的角度解释了相位导数的均值决定了时程峰值的大致发生时刻,相位导数的方差决定了强震段的持续时间。本文改进了均匀调制非平稳过程的相位导数概率密度函数计算公式中强度谱矩的计算方法,使之能够适用于一般非平稳时程。在模拟与指定地震记录相关的非平稳地震动场方法中,计算指定地震记录相位导数的概率密度函数,并按照这一概率密度函数生成其他各点的相位导数,得到其他各点的随机相位谱;然后采用基于功率谱表示的地震动场合成方法,利用快速傅立叶变换技术生成地震动时程。

Abstract

The non-stationary characteristics of an earthquake ground motion are dependent on the phase difference spectrum, which is proportional to the phase derivatives. As viewed from the energy of acceleration time history, the time of PGA is related to the mean value of the phase derivatives while the duration of strong ground motion is related to the variance of the phase derivatives. The intensity moment formula of uniformly modulated random process is modified in this paper in order that the modified formula is applicable to the general non-stationary process. In the process of simulating the non-stationary earthquake ground motion field correlated to a specified earthquake record, the probability density function of phase derivatives for the specified earthquake record is calculated; then both the phase derivatives and the random phase spectrums of the synthesized ground motions are generated. The simulated ground motions, expressed as a function of the power spectrum, coherence function and random phase angles, are generated by discrete Fourier transform.

关键词

地震动场模拟 / 指定地震记录 / 相位差谱 / 相位导数

Key words

simulation of ground motions / specified earthquake record / phase difference spectrum / phase derivatives

引用本文

导出引用
杨娜 田玉基 杨庆山. 与指定地震记录相关的非平稳地震动场的模拟[J]. 振动与冲击, 2012, 31(19): 36-39
Na Yang;Yu;ji TIAN and Qing;shan YANG. Artificial Ground Motions Correlated to a Specified Earthquake Record[J]. Journal of Vibration and Shock, 2012, 31(19): 36-39

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