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Table 1 Characteristics of the base hypothetical model [after Plaksina et al. (2011)]

From: Response surface method for assessing energy production from geopressured geothermal reservoirs

Properties Base value Unit
Temperature of top cell 135 C
Matrix compressibility \(2.0\times 10^{-5}\) \(\mathrm {kPa^{-1}}\)
Dip angle 15 Degree
Reservoir length 2000 m
Cross-section width 100 m
Reservoir thickness 30 m
Permeability 300 md
Porosity 0.2
Rock heat capacity \(2.6\times 10^6\) \(\mathrm {J/(m^3C)}\)
Rock bulk density 2.3 \(\mathrm {g/cm^3}\)
Thermal heat conductivity 172, 800 \(\mathrm {J/(m\,day\,C)}\)
Water thermal expansion \(8.8\times 10^{-4}\) \(\mathrm {C^{-1}}\)
Water compressibility \(4.5\times 10^{-7}\) \(\mathrm {kPa^{-1}}\)
Water molecular weight 0.01802 \(\mathrm {kg/gmol}\)
Water molar density 55, 500 \(\mathrm {gmol/m^3}\)
Water density 1.02 \(\mathrm {g/cm^3}\)
  1. Factors shown by italic are used in the experimental design