Science – Society – Technology
From: Fluid pressure drops during stimulation of segmented faults in deep geothermal reservoirs
Parameter | Description | Value | Source |
---|---|---|---|
E 0 | Mechanical aperture | 1200 µm | |
σ Enref | Reference normal traction (mechanical aperture) | 25 MPa | |
E res | Residual mechanical aperture | 2 µm | |
φ Edil | Dilatation angle (mechanical aperture) | 0°/2.5°/5° | |
e 0 | Hydraulic aperture | 120 µm | |
σ enref | Reference normal traction (hydraulic aperture) | 25 MPa | |
e res | Residual hydraulic aperture | 0.2 µm | |
φ Edil | Dilatation angle (hydraulic aperture) | 2.5° | Arbitrary (good coupling) |
ρ | Fluid density | 1000 kg/m3 | Water values at 20 °C |
µ | Fluid viscosity | 0.001 Pa s | |
h | Out-of-plane dimension | 100 m | To obtain representative magnitudes |
η | Radiation damping coefficient | 3 MPa/(m∕s) | Arbitrary (common value) (McClure 2012) |
S 0 | Cohesion | 0 MPa | Assumption |
G | Shear modulus | 15 GPa | Arbitrary (common value) |
ν r | Poisson’s ratio | 0.25 | Arbitrary (common value) |
f 0 | Nominal friction coefficient | 0.85 | |
d c | Characteristic displacement scale | 100 µm | Gouge material (Marone and Scholz 1988; Scholz 2002; Gischig 2015) |
a | Velocity effect coefficient | 0.01 | Scholz (2002) |
b | State effect coefficient | 0.02 | |
v 0 | Reference velocity | 10−6 m∕s | Arbitrary (common value) |
θ RS | State | 2.6·106 s | |
T str | Matrix tension strength | 3 MPa | Arbitrary (common value)(McClure 2014) |
K1crithf | Stress intensity factor | 1.5 MPa m1/2 | Arbitrary (common value)(Zeeb and Konietzky 2015; Meyer et al. 2017) |