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Ejection velocity v i (m/s) as a function of confining pressure (5, 50 MPa) at the source, calculated using Fagents and Wilson (1993).
Compressional and shear wave velocities in a dry sample (AJG02) are shown as a function of confining pressure in Fig. 3.
By using the estimated crack density parameter, the compressional and shear wave velocities were calculated as a function of confining pressure for the saturation degrees of 80, 90, and 100%% (Fig. 8).
Compressional and shear wave velocities and electrical conductivity are shown in Fig. 6 as a function of confining and pore-fluid pressures.
Velocities and conductivity are shown as a function of confining pressure at different pore-fluid pressures (in MPa; see labels).
The estimated crack density parameter in Sample AJG02 is shown in Fig. 7 as a function of confining pressure.
Volumetric strain in a dry rock sample (AJG07) is shown in Fig. 4 as a function of confining pressure.
Fig. 4 Volumetric strain of dry rock sample AJG07 as a function of confining pressure.
Fig. 7 Crack density parameter in dry sample AJG02 as a function of confining pressure.
Electrical conductivity was measured in brine-saturated sample AJG04 as a function of confining pressure.
Compressional and shear wave velocities and electrical conductivity are shown in Fig. 5 as a function of confining pressure.
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