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Displacements, damage measures and response spectra obtained from a synthetic accelerogram processed by causal and acausal Butterworth filters

机译:由因果和因果巴特沃斯滤波器处理的合成加速度图获得的位移,损伤测度和响应谱

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The aim of this study is to investigate the reliability of strong motion records processed by causal and acausal Butterworth filters in comparison to the results obtained from a synthetic accelerogram. For this purpose, the fault parallel component of the Bolu record of the Duzce earthquake is modeled with a sum of exponentially damped sinusoidal components. Noise-free velocities and displacements are then obtained by analytically integrating the synthetic acceleration model. The analytical velocity and displacement signals are used as a standard with which to judge the validity of the signals obtained by filtering with causal and acausal filters and numerically integrating the acceleration model. The results show that the acausal filters are clearly preferable to the causal filters due to the fact that the response spectra obtained from the acausal filters match the spectra obtained from the simulated accelerogram better than that obtained by causal filters. The response spectra are independent from the order of the filters and from the method of integration (whether analytical integration after a spline fit to the synthetic accelerogram or the trapezoidal rule). The response spectra are sensitive to the chosen corner frequency of both the causal and the acausal filters and also to the inclusion of the pads. Accurate prediction of the static residual displacement (SRD) is very important for structures traversing faults in the near-fault regions. The greatest adverse effect of the high pass filters is their removal of the SRD. However, the noise-free displacements obtained by double integrating the synthetic accelerogram analytically preserve the SRD. It is thus apparent that conventional high pass filters should not be used for processing near-fault strong-motion records although they can be reliably used for far-fault records if applied acausally. The ground motion parameters such as ARIAS intensity, HUSID plots, Housner spectral intensity and the duration of strong-motion are found to be insensitive to the causality of filters.
机译:这项研究的目的是与由合成加速度图获得的结果相比,研究因果和因果的Butterworth滤波器处理的强运动记录的可靠性。为此,用指数衰减的正弦曲线分量的总和对Duzce地震的Bolu记录的断层平行分量进行建模。然后,通过对综合加速度模型进行分析积分,可以获得无噪声的速度和位移。解析速度和位移信号用作判断通过因果和非因果滤波器滤波并在数值上集成加速度模型获得的信号的有效性的标准。结果表明,由于从因果滤波器获得的响应光谱与从模拟加速度图获得的光谱比由因果滤波器获得的光谱更好地匹配,因此因果滤波器明显优于因果滤波器。响应谱与滤波器的阶数和积分方法(无论样条拟合到合成加速度图或梯形规则后的分析积分)无关。响应频谱对因果滤波器和非因果滤波器的所选转折频率敏感,也对焊盘的包含敏感。静态残余位移(SRD)的准确预测对于穿越断层附近断层的结构非常重要。高通滤波器的最大不利影响是它们去除了SRD。但是,通过对合成加速度图进行两次积分获得的无噪声位移在分析上保留了SRD。因此很明显,常规的高通滤波器不应该用于处理近断层强运动记录,尽管如果因果使用它们可以可靠地用于远断层记录。发现诸如ARIAS强度,HUSID图,Housner光谱强度和强运动持续时间等地面运动参数对滤波器的因果关系不敏感。

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