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Seismic Response Analysis of Different Buildings using Time- Invariant and Time- Variant Damping Coefficients

机译:不同建筑物使用时间不变和时变阻尼系数的地震反应分析

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Seismic signals are characterized by strong excitations, short durations, non-linearity and non-stationarity having both the amplitude and frequency content vary as a function of the recorded time. Various classical detection and estimation techniques, like the time-frequency representations and the Fourier-based techniques have been used, to analyze such signals, but these techniques have variety of limitations and they fail to correctly estimate the concerned signals. The Damped-Amplitude and Polynomial-Frequency Model has been introduced to help in adapting to the seismic signals where the amplitude is damped. This model is based on approximating the frequency by low-order polynomials and the amplitude by damped exponentials. Its amplitude in turn is characterized by a damping coefficient; which was firstly assumed to be time-invariant. However the results of the studied signals showed rapid amplitude fluctuations and frequency content variations of each component that could be justified by the fact that the dynamic response of the structure is highly sensitive to the dynamic characteristics of the ground motion. Accordingly and to be more adapted with the physical model of the building motion that is characterized by damped exponential functions, the damping coefficient was then assumed to be time-variant leading to the foundation of a new model that keeps the same approximation for the frequency like the aforementioned model, and changes that of the amplitude by approximating its damping-coefficient by low-order polynomials. This model was then named Polynomial Damping Function Model. Results on different seismic signals show that the time-variant assumption is more efficient than the time-invariant one.
机译:地震信号的特征在于具有幅度和频率内容的强烈激励,短持续时间,非线性和非公平性,其幅度和频率内容都随着记录的时间而变化。已经使用了各种经典检测和估计技术,如已经使用时频表示和基于傅立叶的技术,以分析这些信号,但这些技术具有各种限制,并且它们无法正确估计有关信号。已经引入了阻尼幅度和多项式模型,以帮助调整振幅被阻尼的地震信号。该模型基于近似频率通过衰减指数的低位多项式和幅度。其振幅反过来的特点是阻尼系数;首先认为是时间不变的。然而,所研究信号的结果显示了每个组件的快速幅度波动和频率内容变化,其可以由结构的动态响应对地面运动的动态特性非常敏感。因此,并且更适合于由阻尼指数函数表征的构建运动的物理模型,然后假设阻尼系数是导致新模型的基础的时变量,其保持频率相同的近似上述模型,并通过近似其阻尼系数通过低位多项式来改变幅度的变化。然后将该模型命名为多项式阻尼功能模型。结果不同地震信号表明,时间 - 变体假设比不变量的假设更有效。

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