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Estimation of phase velocity and attenuation coefficient in gas-charged sediment

机译:气带沉积物中相速度和衰减系数的估计

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Anderson-Hampton theory describes the characteristics of gas-charged sediment,near resonance frequency,dispersion in gas-charged sediment causes abnormal high attenuation and high phase velocity.The accurate calculation of attenuation coefficient and phase velocity could estimate physical properties of gas-charged sediment.We propose a method to measure attenuation coefficient and phase velocity from two waveforms propagating at different distances.The synthetic waveform is processed by filter-cross correlation method and spectral ratio to verify validity of proposed method.The characteristics of gas-charged sediment distort waveform,which seriously reduces the accuracy of phase velocity calculation,but the estimation of attenuation is more stable.We focus on the calculation of attenuation to estimate resonance frequency by Anderson-Hampton model.
机译:Anderson-Hampton理论描述了气带沉积物的特性,近共振频率,气管沉积物中的分散导致异常的高衰减和高相速度。衰减系数和阶段速度的精确计算可以估算气带沉积物的物理性质。 .we提出一种方法来测量在不同距离在不同距离传播的两个波形中测量衰减系数和相位速度的方法。通过滤波交叉相关方法和光谱比处理合成波形,以验证提出的方法的有效性。气管沉积物的特性扭曲波形,这严重降低了相速度计算的准确性,但衰减的估计更稳定。我们专注于Anderson-Hampton模型估计谐振频率的衰减计算。

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