工程场址复杂波场特征的确定性分析

DETERMINISTIC ANALYSIS OF WAVEFIELD CHARACTERISTICS AT ENGINEERING SITE

  • 摘要: 工程结构地震响应受场址入射波的直接影响,鲜见工程场址波场特征的相关研究。该文结合地壳速度模型和场地参数提出震源-场址传播介质构建方案,基于空间演化法分析典型工程场址波场的确定性特征,揭示波场信息随震源深度、场址震中距和场地参数的变化规律。研究显示,震源地震波形成的场址入射波数量多且信息复杂。在幅值方面,大幅值数量少,小幅值数量多;幅值随震源深度和场地弹性模量的增加而减小;大幅值随场址震中距的增加而减小、小幅值可能呈现相反规律。入射角为有界分布的小角度入射;同位震源形成的4类入射波中,入射角下限接近且数值较小,入射角上限满足\theta_\mathrmc^\mathrmSP >\theta_\mathrmc^\mathrmSS ≈\theta_\mathrmc^\mathrmPP >\theta_\mathrmc^\mathrmPS ;入射角分布范围随震源深度的增加逐渐减小,随场址震中距和地基弹性模量的增加逐渐增大。在到时方面,4类入射波的最小到时满足t_\mathrmf^\mathrmPP <t_\mathrmf^\mathrmPS <t_\mathrmf^\mathrmSP <t_\mathrmf^\mathrmSS ;入射波在头部聚集、在尾部稀疏,到时范围为15.2 s~31.8 s,与实测地震记录宏观特征一致。

     

    Abstract: The seismic response of engineering structures is directly influenced by incident site waves, while there are few relevant investigations on the wavefield characteristics. To solve this problem, a source-site medium construction scheme combining the Crust1.0 model and the site condition is developed. The deterministic analysis of the wavefield characteristics at typical engineering sites is performed, and the changes in wavefield information with the source depth, with the epicenter distance, and with the site condition are revealed. The result shows that the incident site waves are numerous and with complex information. There are a small number of large amplitude waves and a large number of small amplitude ones. The wave amplitude decreases with the source depth and the elastic modulus of sites. The large amplitude decreases and the small one may increase with the epicenter distance. The site waves are all with small incident angles distributed in a certain range. For four types of waves formed by the source at the same location, the lower limit is small and the upper limit meets \theta_\mathrmc^\mathrmSP >\theta_\mathrmc^\mathrmSS ≈\theta_\mathrmc^\mathrmPP >\theta_\mathrmc^\mathrmPS . The range of incident angles decreases with the source depth and increases with the epicenter distance and the elastic modulus of sites. For four types of waves, the minimum arrival times meet t_\mathrmf^\mathrmPP <t_\mathrmf^\mathrmPS <t_\mathrmf^\mathrmSP <t_\mathrmf^\mathrmSS . The arrival times gather at the head and disperse at the tail, with the range from 15.2 s to 31.8 s. These factors agree well with the characteristics of actual earthquake records.

     

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