地震地面运动局部谱密度的小波变换估计

ESTIMATION OF LOCAL SPECTRAL DENSITY OF EARTHQUAKE GROUND MOTION BASED ON WAVELET TRANSFORM

  • 摘要: 已有的不少研究表明,地震地面运动的时频非平稳特性对结构响应有着很大的影响,对这种影响考虑的准确与否直接涉及结构分析的安全性。因此采用能反映时频非平稳特性的时变谱密度(即局部谱密度)来描述地震地面运动是非常必要的。首先从理论上比较了几种局部谱密度的估计方法,指出利用小波变换来估计局部谱密度在精度和速度方面有着相当的优势,有利于局部谱密度在地震动模型化、结构随机响应分析以及动力可靠度评价等方面的应用。然后通过具体算例,对理论分析进行了验证。

     

    Abstract: Some research results have shown that the non-stationary characteristics of earthquake ground motion influence the structural responses greatly and to take into account the non-stationary characteristics is essential to the structural analysis. Consequently, it is necessary to describe earthquake ground motion with local spectral density, which is time-dependent and can reflect the non-stationary characteristics. Comparisons of estimating precision and speed were firstly carried out in theory among several local spectral density estimation methods, i.e., wavelet transform, multifilter and short time Fourier transform. Some numerical examples were evaluated to validate the theoretical results. It is concluded that wavelet transform has great advantages on local spectral density estimation due to its higher precision and faster speed than that of the other two methods. Based on wavelet transform, it is convenient and efficient to apply local spectral density to many aspects of earthquake engineering, such as earthquake ground motion modeling, structural random response analysis and reliability evaluation under earthquake excitations.

     

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