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Stochastic simulation of fully nonstationary aftershock ground motions from known preceding main shock

机译:来自已知先震的完全非平稳余震地面运动的随机模拟

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Aftershocks can cause significant additional damage to a structure that already got damaged during the preceding main shock. Past studies showed that the ground motion characteristics of an aftershock, in statistical sense, are related to those of the preceding main shock. Hence, statistical assessment of additional damage during future aftershocks given a main shock requires conditional simulation of aftershock ground motions. In the present study, a methodology is proposed to obtain an ensemble of fully nonstationary aftershock ground motions at a site of interest from the known seismic scenarios of both the main shock and the anticipated aftershock. The proposed method is based on the Priestley process assumption in order to characterize both amplitude and frequency nonstationarities via some frequency-dependent deterministic amplitude modulations. The amplitude modulations of a probable aftershock process belonging to the anticipated aftershock seismic scenario are considered to be statistically dependent on those of the recorded main shock process. Since the amplitude modulation is obtained from the frequency-dependent energy arrival curves, a conditional scaling model for the energy arrival of aftershocks is newly proposed. An improved methodology is also proposed in order to extract the frequency-dependent amplitude modulations from the energy arrival curves, obtained either via the scaling model or from a recorded motion, as well as to generate process-specific random samples from the knowledge of such modulations. It is found that the simulated ground motion ensemble shows better agreement with the recorded aftershock process, especially for larger aftershocks, when the aftershock's dependency on its main shock (via the conditional scaling model) is considered than what it shows when the dependency is not considered.
机译:余震可能会对在先前的主冲击中已经损坏的结构造成严重的额外损坏。过去的研究表明,从统计意义上讲,余震的地面运动特征与前一次主震的特征有关。因此,在给定主震的情况下,对未来余震造成的额外破坏进行统计评估需要对余震地面运动进行有条件的模拟。在本研究中,提出了一种方法,该方法可从已知的主震和预期余震的地震场景中,获取感兴趣地点发生的完全非平稳余震地面运动的合奏。所提出的方法基于Priestley过程假设,以便通过一些依赖于频率的确定性幅度调制来表征幅度和频率的非平稳性。属于预期余震地震场景的可能余震过程的振幅调制被认为在统计上取决于所记录的主震过程的振幅调制。由于从与频率相关的能量到达曲线中获得了幅度调制,因此新提出了余震能量到达的条件缩放模型。还提出了一种改进的方法,以便从能量到达曲线提取频率相关的幅度调制,该能量到达曲线既可以通过缩放模型获得,也可以通过记录的运动获得,并且可以根据这种调制的知识生成特定于过程的随机样本。发现在考虑了余震对主震的依赖(通过条件缩放模型)的情况下,模拟的地面运动集合与所记录的余震过程显示出更好的一致性,特别是对于较大的余震,这比不考虑依赖项时所显示的结果更好。 。

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