Modeling of fluid and heat flow in fractured geothermal reservoirs

Conference · Mon Aug 01 00:00:00 EDT 1988

OSTI ID:6782599

Pruess, K

In most geothermal reservoirs large-scale permeability is dominated by fractures, while most of the heat and fluid reserves are stored in the rock matrix. Early-time fluid production comes mostly from the readily accessible fracture volume, while reservoir behavior at later time depends upon the ease with which fluid and heat can be transferred from the rock matrix to the fractures. Methods for modeling flow in fractured porous media must be able to deal with this matrix-fracture exchange, the so-called interporosity flow. This paper reviews recent work at Lawrence Berkeley Laboratory on numerical modeling of nonisothermal multiphase flow in fractured porous media. We also give a brief summary of simulation applications to problems in geothermal production and reinjection. 29 refs., 1 fig.

• Research Organization: Lawrence Berkeley Lab., CA (USA)
• DOE Contract Number: AC03-76SF00098
• OSTI ID: 6782599
• Report Number(s): LBL-25710; CONF-881170-1; ON: DE88016636
• Resource Relation: Conference: International symposium on geothermal energy, Kumamoto, Japan, 10 Nov 1988; Other Information: Portions of this document are illegible in microfiche products
• Country of Publication: United States
• Language: English

Related Subjects

15 GEOTHERMAL ENERGY
99 GENERAL AND MISCELLANEOUS//MATHEMATICS, COMPUTING, AND INFORMATION SCIENCE
GEOTHERMAL FLUIDS
MATHEMATICAL MODELS
FLUID FLOW
GEOLOGIC FRACTURES
GEOTHERMAL ENERGY
GEOTHERMAL SYSTEMS
GEOTHERMAL WELLS
HEAT FLOW
HEAT TRANSFER
NUMERICAL DATA
PERMEABILITY
POROSITY
DATA
ENERGY
ENERGY SOURCES
ENERGY TRANSFER
FLUIDS
GEOLOGIC STRUCTURES
INFORMATION
RENEWABLE ENERGY SOURCES
WELLS
Geothermal Legacy