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Table 1 Summary of the modeling parameters for the cross-validation with benchmark solutions

From: Influence of extreme fracture flow channels on the thermal performance of open-loop geothermal systems at commercial scale

Parameter

Symbol

Values for Fox et al. (2015) validation

Values for Ghassemi et al. (2003) validation

Uniform fracture aperture

b

5 mm

5 mm

Specific heat capacity of the fluid

Cp.f

4184 J/(kg \(\cdot\) K)

4050 J/(kg \(\cdot\) K)

Specific heat capacity of the rock

Cp.r

1000 J/(kg \(\cdot\) K)

1100 J/(kg \(\cdot\)K)

Thermal conductivity of the fluid

kf

0.6 W/(m \(\cdot\) K)

0.6 W/(m \(\cdot\) K)

Thermal conductivity of the rock

kr

2.40 W/(m \(\cdot\) K)

2.58 W/(m \(\cdot\)K)

Dynamic viscosity of the fluid

\(\mu\)

1E-3 Pa \(\cdot\) s

1E-3 Pa \(\cdot\) s

Fluid density

\(\rho\) f

1000 kg/m3

1000 kg/m3

Rock density

\(\rho\) r

2300 kg/m3

2650 kg/m3

Reinjection temperature

Tinj

50 °C

60 °C

Reservoir temperature

Tr

200 °C

140 °C

  1. Values specified in the third and fourth columns correspond to values reported by Fox et al. (2015) and Ghassemi et al. (2003), respectively