Consider a geothermal reservoir (see Figure 32.17) At a depth of 1.5 km, modeled as a cylindrical
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Consider a geothermal reservoir (see Figure 32.17)
At a depth of 1.5 km, modeled as a cylindrical volume of radius r = 5 km and height h = 500m, with pressure at the periphery of pr ≅ 15 MPa, pressure at the bottom of the well of pw ≅ 12 MPa, and permeability of K ≅ 50 mD. Use the answer to Problem 32.6 to estimate the mass flow rate through a well bore of radius rw ≅ 0.125 m. Assume that the fluid is water at roughly 180 ◦C, where the viscosity is η ≅ 0.15 cP.
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