Numerical Calculation Method of Seismic Wave Dispersion and Attenuation Considering Heterogeneous Differences in Seepage of Fractured Pore Rocks
A seismic wave, non-uniform technology, applied in the fields of seismic wave propagation and petrophysics, which can solve problems such as limiting oil and gas seismic exploration applications, difficult to achieve reliable guidance, not considering micro-scale and meso-scale pore space differences and non-uniformity.
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[0021] (1) Given a fracture-porous rock model containing spherical pores, micro-cracks and fractures, the initial velocities of P-wave and S-wave in the background medium of the model are respectively The density of the background medium is ρ o ; In the model, the porosity and radius of spherical pores are: and a p , the density and radius of microcracks are: ε c and a c , the density, radius and aspect ratio of cracks are respectively: ε f , a f and r; in the model, shaped pores and microcracks belong to the microscopic pore space, and their permeability is κ 1 , the fracture belongs to the mesoscale pore space, and the permeability is κ 2 , there are non-uniform differences in the permeability of different scales of pore space inside the rock, then there is κ 1 ≠κ 2 , the bulk modulus of the fluid filled in the pore space is K f ;
[0022] (2) According to the initial velocities of compressional and shear waves in the background medium of the rock model and...
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