This is a pleasant surprise, although the heat is still fairly deep compared to
, but the existence of a huge local market will offset that. The fact is that we can drill fifteen thousand feet in this country pretty consistently. We can even kick out a horizontal leg while we are at it and then fracture rock while down there. Nevada
Placing a parallel well right next to the first horizontal leg could even provide down hole connectivity which means that the injection well can push fluid through the fractures into the recovery well. In this way the actual efficiency of a well pair can be improved many times and a single well pair could provide ample heat flow to supply a power plant.
This would bring down the capital cost per delivered unit of heat fairly dramatically.
I presume that by now, that corrosion issues have been designed out of the technology or at least effectively managed.
The remaining question is whether this heat zone extends the length of the
Appalachians. That it existed at all as an economic resource at a presently reachable depth is unexpected.
The real power of geothermal energy, is that once it is paid for through the first thirty or so years, it operates perpetually and at a very low cost. A society has cheap base energy forever.
SMU Geothermal Finds Large Energy Source In Coal Country
by Staff Writers
New research produced by Southern Methodist University's Geothermal Laboratory, funded by a grant from Google.org, suggests that the temperature of the Earth beneath the state of West Virginia is significantly higher than previously estimated and capable of supporting commercial baseload geothermal energy production.
Geothermal energy is the use of the Earth's heat to produce heat and electricity. "Geothermal is an extremely reliable form of energy, and it generates power 24/7, which makes it a baseload source like coal or nuclear," said David Blackwell,
Professor of Geophysics and Director of the SMU Geothermal Laboratory. Hamilton
The SMU Geothermal Laboratory has increased its estimate of
's geothermal generation potential to 18,890 megawatts (assuming a conservative 2% thermal recovery rate). The new estimate represents a 75 percent increase over estimates in MIT's 2006 "The Future of Geothermal Energy" report and exceeds the state's total current generating capacity, primarily coal based, of 16,350 megawatts. West Virginia
Researchers from SMU's Geothermal Laboratory will present a detailed report on the discovery at the 2010 Geothermal Resources Council annual meeting in
, Oct. 24-27. A summary of the report is available online. Sacramento
The West Virginia discovery is the result of new detailed mapping and interpretation of temperature data derived from oil, gas, and thermal gradient wells - part of an ongoing project to update the Geothermal Map of North America that Blackwell produced with colleague Maria Richards in 2004.
Temperatures below the Earth almost always increase with depth, but the rate of increase (the thermal gradient) varies due to factors such as the thermal properties of the rock formations.
"By adding 1,455 new thermal data points from oil, gas, and water wells to our geologic model of
, we've discovered significantly more heat than previously thought," Blackwell said. West Virginia
"The existing oil and gas fields in
provide a geological guide that could help reduce uncertainties associated with geothermal exploration and also present an opportunity for co-producing geothermal electricity from hot waste fluids generated by existing oil and gas wells." West Virginia
The high temperature zones beneath
revealed by the new mapping are concentrated in the eastern portion of the state (Figure 1). Starting at depths of 4.5 km (greater than 15,000 feet), temperatures reach over 150C (300F), which is hot enough for commercial geothermal power production. West Virginia
Traditionally, commercial geothermal energy production has depended on high temperatures in existing subsurface reservoirs to produce electricity, requiring unique geological conditions found almost exclusively in tectonically active regions of the world, such as the western
. Newer technologies and drilling methods can be used to develop resources in wider ranges of geologic conditions. Three non-conventional geothermal resources that can be developed in areas with little or no tectonic activity or volcanism such as United States are: West Virginia
+ Low-Temperature Hydrothermal - Energy is produced from areas with naturally occurring high fluid volumes at temperatures ranging from 80C (165F) to 150C (300F) using advanced binary cycle technology. Low-Temperature systems have been developed in Alaska, Oregon, and
+ Geopressure and Co-produced Fluids Geothermal - Oil and/or natural gas produced together with hot geothermal fluids drawn from the same well. Geopressure and Co-produced Fluids systems are currently operating or under development in Wyoming, North Dakota, Utah, Louisiana, Mississippi, and
+ Enhanced Geothermal Systems (EGS) - Areas with low natural rock permeability but high temperatures of more than 150C (300F) are "enhanced" by injecting fluid and other reservoir engineering techniques. EGS resources are typically deeper than hydrothermal and represent the largest share of total geothermal resources.
EGS is being pursued globally in Germany, Australia, France, the United Kingdom, and the
U.S. EGS is being tested in deep sedimentary basins similar to West Virginia's in Germany and . Australia
research is very promising," Blackwell said, "but we still need more information about local geological conditions to refine estimates of the magnitude, distribution, and commercial significance of their geothermal resource." West Virginia
Zachary Frone, an SMU graduate student researching the area said, "More detailed research on subsurface characteristics like depth, fluids, structure and rock properties will help determine the best methods for harnessing geothermal energy in
." West Virginia
The next step in evaluating the resource will be to locate specific target sites for focused investigations to validate the information used to calculate the geothermal energy potential in this study.
The team's work may also shed light on other similar geothermal resources. "We now know that two zones of Appalachian age structures are hot -
West Virginia and a large zone covering the intersection of Texas, Arkansas, and Louisiana known as the region," said Blackwell. Ouachita Mountain
"Right now we don't have the data to fill in the area in between," Blackwell continued, "but it's possible we could see similar results over an even larger area."
Blackwell thinks the finding opens exciting possibilities for the region. "The proximity of
West Virginia's large geothermal resource to east coastpopulation centers has the potential to enhance U.S. energy security, reduce CO2 emissions, and develop high paying clean energy jobs in ," he said. West Virginia
SMU's Geothermal Laboratory conducted this research through funding provided by Google.org's REC initiative, which is dedicated to using the power of information and innovation to advance breakthrough technologies in clean energy.