23 January 2014 from UCRToday Website
enhanced or engineered geothermal systems are being created by pumping cold water into hot dry rocks at 4-5 kilometers depths.
The heated water is pumped up again as hot water or steam from production wells.
In recent decades, considerable effort has been invested in Europe, Australia, the United States, and Japan, with uneven, and typically poor, results.
In 2009 a borehole drilled at Krafla, northeast Iceland, as part of the Icelandic Deep Drilling Project (IDDP), unexpectedly penetrated into magma (molten rock) at only 2,100 meters depth, with a temperature of 900-1,000° C.
The borehole, IDDP-1, was the first in a series of wells being drilled by the IDDP in Iceland
in the search for high-temperature
geothermal resources.
Flow test of the IDDP-1 well at Krafla. Note the transparent superheated steam at the top of the rock muffler. Photo credit: Kristján Einarsson.
In 2009 a borehole drilled at Krafla, northeast Iceland, as part of the Icelandic Deep Drilling Project (IDDP), unexpectedly penetrated into magma (molten rock) at only 2,100 meters depth, with a temperature of 900-1,000° C.
The borehole, IDDP-1, was the first in a series of wells being drilled by the IDDP in Iceland in the search for high-temperature geothermal resources. The January 2014 issue of the international journal Geothermics is dedicated to scientific and engineering results arising from that unusual occurrence.
This issue is edited by Wilfred Elders, a professor emeritus of geology at the University of California, Riverside, who also co-authored three of the research papers in the special issue with Icelandic colleagues.
Accordingly, a steel casing, perforated in the bottom section closest to the magma, was cemented into the well.
The hole was then allowed to heat slowly and eventually allowed to flow superheated steam for the next two years, until July 2012, when it was closed down in order to replace some of the surface equipment.
The January 2014 issue of the journal Geothermics is dedicated to scientific and engineering results arising from the Icelandic Deep Drilling Project. The special issue is edited by UC Riverside’s Wilfred Elders.
He added that several important milestones were achieved in this project:
Elders explained that in various parts of the world so-called enhanced or engineered geothermal systems are being created by pumping cold water into hot dry rocks at 4-5 kilometers depths.
The heated water is pumped up again as hot water or steam from production wells.
In recent decades, considerable effort has been invested in Europe, Australia, the United States, and Japan, with uneven, and typically poor, results.
The drill site of the IDDP-1 well near the explosive volcanic crater Víti. Viti erupted in 1724 AD. Photo credit: Guđmundur Ó. Friđleifsson.
The IDDP is a collaboration of three energy companies:
...and a government agency, the National Energy Authority of Iceland.
It will drill the next borehole, IDDP-2, in southwest Iceland at Reykjanes in 2014-15.
From the onset, international collaboration has been important to the project, and in particular a consortium of U.S. scientists, coordinated by Elders, has been very active, authoring several research papers in the special issue of Geothermics.
Funding for the science program of the IDDP was provided by the U.S. National Science Foundation (NSF) and the International Continental Scientific Drilling Program.
The Krafla geothermal power plant Source: ucdavis.edu
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