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Identification of Soil-Foundation Dynamic Stiffness from Seismic Response Signals

机译:从地震响应信号识别土基动力刚度

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Prediction of the seismic response of civil structures without considering the flexibility and damping provided by their supporting soil-foundation systems can be unrealistic, especially for stiff structures. In engineering practice, the substructure method is generally preferred for considering Soil-Structure Interaction (SSI) due to its computationally efficiency. In this method, soil is modeled using discrete spring elements that are attached to the superstructure; and the Foundation Input Motions (FIMs)-which are usually calculated through analytical transfer functions from recorded/anticipated free-field motions-are applied at the ends of these springs. Whereas the application of the substructure method itself is simple, the determination of FIMs and the soil-foundation systems' dynamic stiffnesses are challenging. In the present study, we propose two new approaches to identify the dynamic stiffness of soil-foundation systems from response signals recorded during earthquakes. In these approaches, the superstructure is represented either by a numerical (finite element) or by an analytical (Timoshenko beam) model, and the soil is represented by discrete frequency-dependent springs. In both approaches, the superstructure and soil-foundation stiffnesses are all identified through model updating. We present various forms for the second approach (involving the Timoshenko beam) and verify these through comparisons with the results from the first approach (involving the finite element model) obtained using earthquake data recorded at the Robert A. Millikan Library at the Caltech campus in Pasadena, CA.
机译:在不考虑土工基础结构支撑系统提供的柔韧性和阻尼的情况下,对土木结构的地震响应进行预测可能是不现实的,尤其是对于刚性结构而言。在工程实践中,考虑到土-结构相互作用(SSI),通常首选子结构方法,因为它的计算效率很高。在这种方法中,土壤是使用附着在上部结构上的离散弹簧单元建模的。在这些弹簧的末端施加了基础输入运动(FIM),通常通过分析传递函数从记录的/预期的自由场运动中计算出基础输入运动(FIM)。尽管子结构方法本身的应用很简单,但是FIM的确定和地基系统的动态刚度却具有挑战性。在本研究中,我们提出了两种新方法,可以根据地震期间记录的响应信号来识别土壤基础系统的动态刚度。在这些方法中,上部结构由数值(有限元)模型或解析(Timoshenko梁)模型表示,而土壤则由离散的频率相关弹簧表示。在这两种方法中,都通过模型更新来识别上部结构和地基刚度。我们介绍了第二种方法(涉及Timoshenko光束)的各种形式,并通过与第一种方法(涉及有限元模型)的结果进行比较,验证了这些形式,这些结果是使用位于加州理工学院的Robert A. Millikan图书馆记录的地震数据获得的加利福尼亚州帕萨迪纳。

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