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Total thermal installed capacity in MWt:
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4,460
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Direct use in TJ/year
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45,301
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Direct use in GWh/year
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12,584.6
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Capacity factor
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0.32
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Heat pumps are the main geothermal use in the country, with the Lund district heating project being the largest geothermal plant producing about 250 GWh/yr, and has been doing so for 25 years.
The majority of the heat pumps are small and typically used in single houses. There are currently around 230,000 installations with about 25,000 units installed annually. Bedrock-soil-water is the most common source for heat pumps using geothermal energy with about 12 TWh of energy extracts or about 15% of the national heat demand covered. A number of systems used underground thermal energy storage UTES), either as aquifer thermal energy storage (ATES) or borehole thermal energy storage (BTES). The former was implemented in the mid 1980s and current there are approximately 100 plants using this system, mainly large scale with average capacity of 2.5 MWt.
Water wells are used and serve a dual function, both as production and injections wells, with the flow direction being reversed from summer to winter. The BTES systems consist of a number of closed spaced boreholes, normally 50 to 200 m deep. These are equipped with borehole heat exchanger, with the holes filled with ground water and not grouted. It has been shown that water filled boreholes are more efficient than grouted ones. These are typically used for combined heat and cooling of commercial and institutional buildings. The reported total for UTES is 90 MWt and 504 TJ/yr for heatings and 90 MWt and 612 TJ/yr for cooling.
For geothermal use in the country the following is listed:
140 MWt and 828 TJ/yr for individual space heating;
90 MWt and 504 TJ/yr for UTES;
4,230 MWt and 43,969 TJ/yr for other geothermal heat pump systems;
for a total of 4,460 MWt and 45,301 TJ/yr, all as geothermal heat pumps.
Taken from the paper by John W. Lund, Derek H. Freeston, and Tonya L. Boyd: "Direct Utilization of Geothermal Energy 2010 Worldwide Review"; published in Proceedings of the World Geothermal Congress 2010, Bali, Indonesia, 25-29 April 2010