Krafla geothermal field, Iceland. II. The natural state of the system

Journal Article · Thu Nov 01 00:00:00 EST 1984 · Water Resour. Res.; (United States)

DOI:https://doi.org/10.1029/WR020i011p01531· OSTI ID:5536186

Bodvarsson, G S; Pruess, K; Stefansson, V; Eliasson, E T

A model of the natural state of the Krafla reservoir system in Iceland has been developed. The model consists of a vertical cross section which includes reservoirs in both old and new well fields. The physical processes considered include mass transport, conductive and convective heat transfer and boiling, and condensation. Natural heat losses to surface manifestations (springs) are also included. The model matches very well all relevant data from the Krafla field. The natural flow of hot fluids through the reservoirs is estimated as approximately 20 kg/s. Steam escaping to surface springs constitutes the bulk of the heat losses in the area modeled. Conductive heat losses through the caprock are approximately 1 W/m/sup 2/, and heat recharge from below is about 2 W/m/sup 2/.

• Research Organization: Univ. of California, Berkeley
• DOE Contract Number: AC03-76SF00098
• OSTI ID: 5536186
• Journal Information: Water Resour. Res.; (United States), Vol. 20:11
• Country of Publication: United States
• Language: English

Related Subjects

15 GEOTHERMAL ENERGY
KRAFLA GEOTHERMAL FIELD
COMPUTERIZED SIMULATION
BOILING
CONVECTION
GEOTHERMAL ENERGY
GEOTHERMAL RESOURCES
ICELAND
MASS TRANSFER
THERMAL CONDUCTION
THERMAL CONDUCTIVITY
DEVELOPING COUNTRIES
ENERGY
ENERGY SOURCES
ENERGY TRANSFER
EUROPE
GEOTHERMAL FIELDS
HEAT TRANSFER
ISLANDS
PHASE TRANSFORMATIONS
PHYSICAL PROPERTIES
RENEWABLE ENERGY SOURCES
RESOURCES
SIMULATION
THERMODYNAMIC PROPERTIES
WESTERN EUROPE
150200* - Geology & Hydrology of Geothermal Systems