Dry-Steam Wellhead Discharges from Liquid-Dominated Geothermal Reservoirs: A Result of Coupled Nonequilibrium Multiphase Fluid and Heat Flow Through Fractured Rock

Dynamic Fluids and Transport Through in Fractured Rock

Volumn , Issue , 2013, Pages 175-181

  Pritchett, John W ^a  

^a SCIENCE APPLICATIONS INTERNATIONAL CORPORATION   (United States)

Author keywords

Groundwater flow Mathematical models; Rocks Permeability Mathematical models

Indexed keywords

ENTHALPY; FRACTURE; GEOTHERMAL FIELDS; GROUNDWATER; GROUNDWATER FLOW; PETROLEUM RESERVOIR ENGINEERING; WELLHEADS;

EXCESS ENTHALPIES; FLUID PRESSURES; FRACTURED ROCK; GEOTHERMAL RESERVOIR; MULTIPHASE FLUIDS; NON EQUILIBRIUM; PERMEABILITY CONTRASTS; VERTICAL DISTRIBUTIONS;

TWO PHASE FLOW;

EID: 84952908480     PISSN: None     EISSN: None     Source Type: Book    
DOI: 10.1029/162GM16     Document Type: Chapter

References (6)

1. Brace, W.R, Permeability of crystalline and argillaceous rocks, Int. J. Rock Mech. Min. Sci, 17, 241-251, 1980.
2. th Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, California, 2000.
3. th Workshop on Geothermal Reservoir Engineering, 61-66, Stanford University, Stanford, California, 1989.
4. nd Workshop on Geothermal Reservoir Engineering, 287-293, Stanford University, Stanford, California, 1997.
5. Pruess, K., and T.N. Narasimhan, On fluid reserves and the production of superheated steam from fractured, vapor-dominated geothermal reservoirs, J. Geophys. Res., 87(B11), 9329-9339, 1982.
6. Tosha, T., N. Matsushima, and T. Ishido (2003), Zeta potential measured for an intact granite sample at temperatures to 200°C, Geophys. Res. Lett, 30(6), 1295, 2003.