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Geothermal Energy Resources and Applications in Iran

Younes Noorollahi, Hossein Yousefi

Key words
Geothermal, Resources, Iran, Direct use
Location
Iran
Conference
World Geothermal Congress
Year
2010
Session
16. Resource Assessment
Language
English
Paper number
1604

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Abstract

In 1975, development of geothermal energy resurces was started by a contract among the Ministry of Energy, ENEL (Entes Nazionale per L’Energia Elettrica) of Italy and TB (Tehran Berkeley) of Iran for exploration in the north-western part. In 1983 the result of investigations defined Sabalan, Damavand, Khoy-Maku and Sahand regions as four prospected geothermal sites in north western Iran.
From 1996 to 1999 a countrywide geothermal energy resource exploration project was carried out by Renewable Energy Organization of Iran (SUNA) and ten more potential areas were indicated additionally. Geothermal potential site selection using Geographic Information System (GIS) was carried out in Kyushu University in 2007. The results indicated 8.8% of Iran as prospected geothermal areas in 18 fields.
Sabalan as a first priority of geothermal potential regions was selected for detailed explorations. Since 1995, surface exploration and feasibility studies have been carried out and five promising areas were defined. Among those prospective areas, NW Sabalan geothermal filed was defined for detailed exploration to justify exploration drilling and to estimate the reservoir characteristics and capacity.
From 2002 to 2004 three deep exploration wells were drilled for evaluation of subsurface geological conditions, geothermal reservoir assessment and response simulation. Two of the wells were successful and a maximum temperature of 240°C at a depth of 3197 m was recorded. As a result of the reservoir simulation, a 55 MW power p lant is projected to be installed in the Sabalan field as a first in geothermal power generation. To supply the required steam for the geothermal power plant (GPP) 17 deep production and reinjection wells are planned to be drilled this year

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