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An Improved Approach for Nonstationary Strong Ground Motion Simulation

机译:一种非平稳强地面运动仿真的改进方法

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摘要

A new stochastic ground motion model for generating a suite of ground motion time history with both temporal and frequency nonstationarities for specified earthquake and site characteristics is proposed based on the wavelet method. This new model is defined in terms of 6 key parameters that characterize the duration, evolving intensity, predominant frequency, bandwidth and frequency variation of the ground acceleration process. All parameters, except for peak ground acceleration (PGA), are identified manually from a database of 2444 recorded horizontal accelerations. The two-stage regression analysis method is used to investigate the inter- and intra-event residuals. For any given earthquake and site characteristics in terms of the fault mechanism, moment magnitude, Joyner and Boore distance and site shear-wave velocity, sets of the model parameters are generated and used, in turn, by the stochastic model to generate strong ground motion accelerograms, which can capture and properly embody the primary features of real strong ground motions, including the duration, evolving intensity, spectral content, frequency variation and peak values. In addition, it is shown that the characteristics of the simulated and observed response spectra are similar, and the amplitude of the simulated response spectra are in line with the predicted values from the published seismic ground motion prediction equations (SGMPE) after a systematic comparison. The proposed method can be used to estimate the strong ground motions as inputs for structural seismic dynamic analysis in engineering practice in conjunction with or instead of recorded ground motions.
机译:基于小波方法,提出了一种新的随机地震动模型,用于生成一整套具有特定时间和频率非平稳性的时间和频率非平稳性的地震动时程。该新模型是根据6个关键参数定义的,这些参数描述了地面加速过程的持续时间,强度变化,主要频率,带宽和频率变化。从2444个记录的水平加速度数据库中手动识别除峰值地面加速度(PGA)以外的所有参数。两阶段回归分析方法用于调查事件间和事件内残差。对于任何给定的地震和场地特征,包括断层机制,弯矩大小,Joyner和Boore距离以及场地剪切波速度,都会生成模型参数集,并由随机模型依次使用这些参数来产生强烈的地面运动加速度图,可以捕捉并适当体现真实的强地面运动的主要特征,包括持续时间,强度变化,频谱含量,频率变化和峰值。此外,在系统比较之后,还显示了模拟和观察到的响应谱的特性相似,并且模拟响应谱的幅度与已发布的地震地震动预测方程(SGMPE)的预测值一致。所提出的方法可以结合或代替记录的地面运动来估计强地面运动,作为工程实践中结构地震动力学分析的输入。

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