1992
DOI: 10.1016/0375-6505(92)90007-v
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Nesjavellir geothermal co-generation power plant

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Cited by 20 publications
(8 citation statements)
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“…The Hengill volcanoes were found in the late 1960s to have high potential for geothermal energy production (Gunnarsson et al, 1992). The natural geothermal activity is expressed by numerous hot springs and fumaroles spread throughout the area around the three central volcanoes (Figure 1), (Saemundsson, 1995;Arnórsson et al, 2008).…”
Section: The Geothermal System At Hengill Volcano Complexmentioning
confidence: 99%
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“…The Hengill volcanoes were found in the late 1960s to have high potential for geothermal energy production (Gunnarsson et al, 1992). The natural geothermal activity is expressed by numerous hot springs and fumaroles spread throughout the area around the three central volcanoes (Figure 1), (Saemundsson, 1995;Arnórsson et al, 2008).…”
Section: The Geothermal System At Hengill Volcano Complexmentioning
confidence: 99%
“…Several geophysical techniques have been applied to study the structure of the Hengill high-temperature area (Bjornsson et al, 1986;Gunnarsson et al, 1992). Within the IGET project, transient electromagnetism (TEM) surveys and 3D magneto-telluric (MT) profiles have been acquired over the area (Árnason et al, 2010).…”
Section: Integrating Velocity and Resistivity Structuresmentioning
confidence: 99%
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“…Two power plants operated by Reykjavík Energy are located at Hengill central volcano in southwestern Iceland (Figure 1). Nesjavellir is a co-generation power plant, where fresh water is heated by geothermal steam in heat exchangers (Gunnarsson et al, 1992). The plant began production in 1990, initially providing hot water mainly for district heating in the capital of Reykjavik, but since 1998 has also been generating electricity.…”
Section: Icelandmentioning
confidence: 99%
“…Although many of these systems have been successfully operated for decades, such as in Iceland, Indonesia, Japan, and New Zealand, the development of potential geothermal resources of this type is geographically restricted to locations with unique geologic characteristics (e.g. volcanic and permeable aquifers) and has a range of aquifer water temperatures ranging from 80 to 150˚C [1][2][3][4][5][6][7]. Capture and use of water/steam from geothermally heated aquifers is not always a renewable resource and most heat reservoirs have a finite lifeexpectancy based on a higher heat harvesting rate vs. the heat flux into the system.…”
Section: Introductionmentioning
confidence: 99%