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Time Frequency Wavenumber Analysis of Surface Waves and Signal Enhancement Using S-Transform

机译:表面波的时频波数分析和信号增强

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摘要

Highly dispersive surface waves resulting from the combination of strong lateral seafloor heterogeneities, shallow water depths and hard sea bottom severely degrade seismic reflection data quality. Considering that seismic signals are nonstationary and surface waves have various spectra over time, we proposed S-transform-based time frequency wavenumber analysis technique which allows the dynamic analysis of spectrum over time. The data is first transformed from the time space domain to the time-wavenumber domain through one-dimensional Fourier transform over the spatial variable, then the variable-factor S-transform is applied over time. Nonstationary filtering is then designed to identify and separate surface waves in complex wavefields, based on its low frequency and low velocity properties, in the time-frequency-wavenumber (TFK) domain. Application to field data illustrates that with this technique, not only is the surface wave effectively suppressed, but also the reflective signals are enhanced, which confirm the validity of the method.
机译:强烈的横向海底非均质性,浅水深度和坚硬的海底相结合产生的高度分散的表面波严重降低了地震反射数据的质量。考虑到地震信号是非平稳的,地表波随时间变化的频谱,我们提出了一种基于S变换的时频波数分析技术,可以对频谱随时间进行动态分析。首先通过空间变量的一维傅立叶变换将数据从时空域转换为时波数域,然后随时间应用变量因子S变换。然后将非平稳滤波设计为基于时频波数(TFK)域中的低频和低速特性,在复杂波场中识别并分离出表面波。在现场数据中的应用表明,采用该技术不仅可以有效地抑制表面波,而且可以增强反射信号,从而证实了该方法的有效性。

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