Method for inverting rock pore distribution characteristics by utilizing pore and fracture medium elastic wave theory
A pore distribution, elastic wave technique, applied in the field of rock physics
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Embodiment 1
[0184] Implementation example 1: Kayenta sandstone (saturated compressional and shear wave velocities)
[0185] First, the core measurement data of Kayenta sandstone (Coyner, 1984) were processed by inversion method. Kayenta sandstone is a high-porosity rock with a porosity of 22.2% and a skeleton density of 2017kg / m 3 , the permeability is taken as 63mD, the sound velocity measurement frequency is 1MHz, and the effective pressure range of the experiment is 1MPa to 70Mpa, Figure 2-a The measured data (circle identifiers) of the variation of P- and S-wave velocities with pressure for the sandstone sample under benzene-saturated conditions are given. The bulk modulus and shear modulus of rock matrix obtained by inversion are 31.00GPa and 24.04GPa, respectively.
[0186] exist Figure 2-a In , the abscissa is the effective pressure (MPa), the ordinate is the velocity (m / s), the black circles are the measured P-wave and S-wave velocities under saturation conditions; the black sol...
Embodiment 2
[0190] Implementation Example 2: Navajo Sandstone (Combined Saturated, Dry P- and S-Wave Velocities)
[0191] Process the core measurement data (Coyner, 1984) of Navajo sandstone with the inversion method of the present invention below, and Navajo sandstone is comparatively compact, and porosity is 11.8%, and skeleton density is 2316kg / m 3 , the frequency of sound velocity measurement is 1MHz, and the effective pressure range of the experiment is from 1MPa to 100MPa. Figure 3-a The measured data (circle identifiers) of the longitudinal and shear wave velocities as a function of pressure under benzene-saturated, dry conditions are given. The difference from Example 1 is that we adopt saturated and dry joint inversion of compressional and shear wave velocities. In particular, for sandstone, in order to better fit the data, we set two rock matrix shear moduli for saturated and dry conditions in the inversion, and the rock matrix bulk modulus and The matrix shear modulus at sat...
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