Seismic signal Q value estimation method based on non-Gaussianity maximization
A seismic signal and Gaussian technology, applied in seismic signal processing, seismology, geophysical measurement, etc., can solve problems affecting attenuation compensation or fluid identification accuracy, reflection coefficient white noise, and Q value estimation accuracy, etc., to achieve effective Good for high resolution, stable Q value distribution, and overcoming instability
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[0039] The steps of the estimation method of seismic signal Q value based on non-Gaussian maximization are as follows:
[0040] (1) Study the attenuation process of seismic signals, and analyze the relationship between attenuation signals and non-Gaussian properties;
[0041] (2) Scan the Q value, in order to avoid the influence of the instability of the amplitude compensation on the non-Gaussian, only do the phase correction;
[0042] (3) Calculate the non-Gaussianity of the phase-corrected seismic signal. When the non-Gaussianity is maximized, a stable quality factor Q value estimation result can be obtained, which serves for subsequent attenuation compensation and reservoir fluid identification.
[0043] Due to the heterogeneity and viscosity of the medium, the signal The absorption decay process can be expressed as:
[0044]
[0045] where H(0,ω) is spectrum, is the seismic signal after amplitude attenuation and phase distortion, Q(t) is the quality factor, ω is ...
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