Predicting method for longitudinal wave speed and attenuation in pore fracture medium
A technology of longitudinal wave velocity and prediction method, applied in the field of seismic rock physics, can solve the problems of not showing the characteristics of cracks and complicated calculation process
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Embodiment 1
[0081] A method for predicting the velocity and attenuation of longitudinal waves in porous and fractured media, comprising the following steps:
[0082] (1) Obtain the experimental data of ultrasonic velocity changing with pressure;
[0083] (2) Establish an equivalent medium theory that conforms to the microscopic pore structure characteristics of porous and fractured reservoirs, and combine the obtained experimental data to obtain the microscopic pore structure characteristics inside the rock;
[0084] (3) Deduce the stress-strain relationship of porous and fractured media;
[0085] (4) Deriving the equation of motion of porous and fractured media;
[0086] (5) By simulating the fracture as a coin-shaped embedded body to simulate the pore fluid flow between pores and fractures, deduce the local flow control equation of the porous and fractured medium;
[0087] (6) Using plane wave analysis to predict the longitudinal wave velocity and attenuation of porous and fractured m...
Embodiment 2
[0142] In this embodiment, a porous and fractured medium model is designed, and the Tang model, DFM model, Gassmann theory and the predicted results of the present invention are compared and analyzed, such as figure 2 shown. The basic petrophysical parameters are: the bulk modulus and shear modulus of rock particles are 37.9 and 32.6GPa respectively, and the density of rock particles is 2650; the bulk modulus of the skeleton is 4.71GPa, and the shear modulus is 4.99GPa; the volume of water Modulus 2.25GPa, density 1000kg / m 3 , viscosity 0.001Pa·s; the local porosity φ of the background phase and the embedded body 10 and φ 20 The permeability is 0.1D and 100D, the skeletal modulus is 7.6 and 0.096GPa, the fracture density is 0.2, the fracture aspect ratio is 0.002, and the fracture radius is 0.0053m. It can be seen from the figure that the P-wave velocity predicted by this note is in good agreement with Gassmann's prediction at low frequencies, and can explain the P-wave di...
Embodiment 3
[0144] In this embodiment, a porous and fractured medium model is designed to analyze the influence of fracture characteristics on the characteristics of longitudinal wave propagation. The basic petrophysical parameters are: the bulk modulus and shear modulus of rock particles are 37.9GPa and 32.6GPa respectively, and the density of rock particles is 2650kg / m 3 ; The bulk modulus of the skeleton is 4.71GPa, the shear modulus of the skeleton is 4.99GPa; the bulk modulus of water is 2.25GPa, and the density is 1000kg / m 3 , viscosity 0.001Pa·s; the local porosity φ of the background phase and the embedded body 10 and φ 20 are 0.25 and 0.32, the permeability is 0.1D and 100D, the skeleton modulus is 7.6 and 0.096GPa, image 3 The crack density is 0.2, the crack aspect ratio is 0.002, and the crack radius is 10- 6 ~0.1m, the schematic diagram of the variation of P-wave velocity and attenuation with fracture radius in seismic frequency band (10Hz), logging frequency band (1000Hz)...
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