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Thursday, February 23, 2006 Tapping Rocks for PowerContinued from page 1 By Peter Fairley
The key to its success to date has been painstaking geological analysis, which ensures they position their wells to hit the right rocks. In 1997, after ten years of work, the project demonstrated impressive flow rates, moving brine heated to 140 degrees Centigrade at a rate of 25 liters per second and a depth of 3.6 kilometers. And the resistance was less than half that encountered at Los Alamos. That positive result emboldened the project's leaders to push their wells deeper, into 200-degree Centigrade granite five kilometers deep -- and last fall they finally turned on the taps. Daniel Fritsch, project coordinator, says the system "could probably do 40 to 50 liters per second" with the addition of pumps that will be installed in the wells this summer -- another kind of technological challenge given the punishing temperatures involved, which few pumps are capable of withstanding. Then the plan is to build a pilot electrical plant by early 2007 to generate 1.5 megawatts, about the same output as one of today's towering wind turbines. But the hot-rock plant won't go idle every time the wind dies down, and should produce about three times more energy per year. Fritsch says that to cover the cost of its equipment and to generate a profit, however, the project should produce closer to five megawatts. To produce more power, however, they must more than double the flow rate, to around 100 liters/second, which could be a challenge due to the large amount of shaking their blasts cause on the surface. Lawsuits from some disgruntled citizens claiming property damage have limited Fritsch's willingness to use stronger hydraulic blasts. To many local people, though, it seems like much ado about nothing. Local journalist Bernard Stéphan, who lives two kilometers from the project's ground zero, says his home has not been affected by the blasts. And Soultz-sous-Fôrets mayor Alfred Schmitt says "There is no problem." Nevertheless, instead of using stronger hydraulic blasts to open the rocks further, Fritsch plans to complement the blasting with a new method: pouring acid in the wells. The idea is to dissolve salt deposits in the fractures immediately surrounding the wells. Fritsch says that tests in Italy with acid have improved the functioning of some geothermal wells by a factor of 10. Peter Fairley is a Technology Review contributing writer based in Paris. |
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Oceans of Power
08/13/2001
Massachusetts Institute of Technology
Comments
Guest (SirLanse) on 02/23/2006 at 12:00 AM
1
You don't do business with plaintiffs.
Guest (Mike) on 02/23/2006 at 12:00 AM
1
Side Question - does anyone have a URL that shows bedrock temps here in the U.S.?
Guest (Fred Singer) on 02/23/2006 at 12:00 AM
1
How is this factored into the cost of the electric power produced?
singer@sepp.org
Guest (geoff) on 02/24/2006 at 12:00 AM
1
Guest (Ted Anderson) on 02/24/2006 at 12:00 AM
1
I am still unclear about how long the heat can be removed from a system of well before the stored heat is depleted. What is the lifetime of one of these wells? Does heat flow in from the neighboring rock? If so it would limit how close together well could be sited.
Guest (Emanuel) on 02/27/2006 at 12:00 AM
1
What's the efficiency of the entire enterprise?
Guest (jh) on 04/27/2006 at 12:00 AM
1