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Estimation of Frequency Dependent Attenuation of Seismic Wave in Time-Frequency Domain Based on Continous Wavelet Transform (CWT)

机译:基于连续小波变换(CWT)时频域地震波频率相关衰减的估计

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Frequency dependent attenuation of seismic waves that propagate through the partially fluid saturated porous rock will be observed. The new method for estimation of frequency dependent attenuation will be developed. The frequency dependent attenuation will be calculated in time-frequency domain which obtained using a spectral decomposition method based on continuous wavelet transform (CWT). The attenuation estimation method will be applied to synthetic data of reflection seismic and vertical seismic profiling (VSP) which were obtained from numerical modeling of seismic wave propagation in partially fluid saturated porous medium using parallel processing technologies based on the Graphics Processing Unit (GPU). The synthetic data of reflection seismic and vertical seismic profiling (VSP) will be transformed to time-frequency domain using continuous wavelet transform (CWT). The frequency dependent attenuation will be calculated in time-frequency domain. The result of attenuation estimation indicates that the maximum value of attenuation is present at varying frequencies and correlated with the physical properties of the partially fluid saturated porous rock.
机译:将观察通过部分流体饱和多孔岩石传播通过部分流体饱和多孔岩石的地震波的频率依赖性衰减。将开发出估计频率相关衰减的新方法。频率相关衰减将在使用基于连续小波变换(CWT)的频谱分解方法获得的时频域中计算。衰减估计方法将应用于反射地震和垂直地震分析(VSP)的合成数据,其根据图形处理单元(GPU)使用平行处理技术在部分流体饱和多孔介质中的地震波传播中的数值模拟中获得。反射地震和垂直地震分析(VSP)的合成数据将使用连续小波变换(CWT)转换为时频域。频率相关的衰减将在时频域中计算。衰减估计的结果表明,衰减的最大值以不同的频率存在并与部分流体饱和多孔岩的物理性质相关。

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