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Wavelet Energy Spectrum for Time-Frequency Localization of Earthquake Energy

机译:小波能谱用于地震能量的时频定位

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The authors recently developed a method for time-frequency signal analysis of earthquake records using Mexican hat wavelets. Ground motions in earthquakes are postulated as a sequence of simple penny-shaped ruptures at different locations along a fault line and occurring at different times. In this article, a wavelet energy spectrum is proposed for time-frequency localization of the earthquake input energy. The ground acceleration generated by a simple penny-shaped rupture is used as the basis to form the mother wavelet. The symmetric Mexican hat wavelet is chosen as the mother wavelet. The spectrum is presented pictorialiy in a two-dimensional, time-frequency domain. The proposed wavelet energy spectrum can be used to observe the evolution of the frequency contents of earthquake energy over time and distance of the site from the epicenter in a more accurate manner than the traditional time series (accelerogram) or frequency domain (Fourier amplitude spectrum) representation. It can be viewed as a microscope for looking into the time-frequency characteristics of earthquake acceleration records. The wavelet energy spectrum provides frequency evolution information to be used in the structural design process.
机译:作者最近开发了一种使用墨西哥帽小波对地震记录进行时频信号分析的方法。地震中的地震动被假定为沿着断层线的不同位置且发生在不同时间的一系列简单的便士形破裂。本文提出了一种小波能谱,用于地震输入能量的时频定位。由简单的便士形破裂产生的地面加速度被用作形成母子波的基础。选择对称的墨西哥帽小波作为母小波。频谱在二维时频域中以图形方式显示。与传统的时间序列(加速度图)或频域(傅立叶振幅谱)相比,所提出的小波能谱可用于以更准确的方式观察地震能量的频率内容随时间和站点距震中的距离的变化。表示。可以将其视为观察地震加速度记录的时频特征的显微镜。小波能谱提供了在结构设计过程中使用的频率演化信息。

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