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| url =http://geoheat.oit.edu/bulletin/bull25-3/art2.pdf
| url =http://geoheat.oit.edu/bulletin/bull25-3/art2.pdf
| issn =0276-1084
| issn =0276-1084
| accessdate =2009-04-13}}</ref> following the [[1970s energy crisis]] and significant changes in regulatory policies. This technology allows the use of much lower temperature resources than were previously recoverable. In 2006, a binary cycle plant in [[Chena Hot Springs, Alaska]], came on-line, producing electricity from a record low fluid temperature of 57°C (135°F).<ref name="Chena"/>
| accessdate =2009-04-13}}</ref> following the [[1970s energy crisis]] and significant changes in regulatory policies. This technology allows the use of much lower temperature resources than were previously recoverable. In 2006, a binary cycle plant in [[Chena Hot Springs, Alaska]], came on-line, producing electricity frntil recently been built exclusively where high temperature geothermal resources are available near the surface. The development of [[binary cycle power plant]]s and improvements in drilling and extraction technology may enable [[enhanced geothermal systems]] over a much greater geographical range.<ref name="INEL" /> Demonstration projects are operational in [[Landau-Pfalz]], Germany, and [[Soultz-sous-Forêts]], France, while an earlier effort in [[Basel]], Switzerland was shut down after it triggered earthquakes. Other demonstration projects are under construction in [[Geothermal power in Australia|Australia]], the [[United Kingdom]], and the [[United States of America]].<ref>{{Citation

Geothermal electric plants have until recently been built exclusively where high temperature geothermal resources are available near the surface. The development of [[binary cycle power plant]]s and improvements in drilling and extraction technology may enable [[enhanced geothermal systems]] over a much greater geographical range.<ref name="INEL" /> Demonstration projects are operational in [[Landau-Pfalz]], Germany, and [[Soultz-sous-Forêts]], France, while an earlier effort in [[Basel]], Switzerland was shut down after it triggered earthquakes. Other demonstration projects are under construction in [[Geothermal power in Australia|Australia]], the [[United Kingdom]], and the [[United States of America]].<ref>{{Citation
| first = Ruggero | last = Bertani
| first = Ruggero | last = Bertani
| contribution = Geothermal Energy: An Overview on Resources and Potential
| contribution = Geothermal Energy: An Overview on Resources and Potential
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| place = Slovakia}}</ref>
| place = Slovakia}}</ref>


The [[thermal efficiency]] of geothermal electric plants is low, around 10-23%,<ref>http://gafoen.com/site/index.php?page=geothermalenergy</ref> because geothermal fluids are at a low temperature compared with steam from boilers. By the laws of [[thermodynamics]] this low temperature limits the efficiency of [[Heat engine#Efficiency|heat engines]] in extracting useful energy during the generation of electricity. Exhaust heat is wasted, unless it can be used directly and locally, for example in greenhouses, timber mills, and district heating. The efficiency of the system does not affect operational costs as it would for a coal or other fossil fuel plant, but it does factor into the viability of the plant. In order to produce more energy than the pumps consume, electricity generation requires high temperature geothermal fields and specialized heat cycles.{{Citation needed|date=May 2010}} Because geothermal power does not rely on variable sources of energy, unlike, for example, wind or solar, its [[capacity factor]] can be quite large – up to 96% has been demonstrated.<ref>{{Citation
The [[thermal efficiency]] of geothermal electric plants is low, around 10-23%,<ref>http://gafoen.com/site/index.php?page=geothermalenergy</ref> because geothermal fluids are at a low temperature compared with steam from boilers. By the laws of [[thermodynamics]] this low temperature limits the efficiency of [[Heat engine#Efficiency|heat engines]] in extracting useful energy during the generation of electricity. WOW!!!!!!!!!!!!!!!!!
| last = Lund | first = John W.
| title = The USA Geothermal Country Update
| journal = Geothermics | volume = 32 | issue = 4-6
| pages = 409–418
| publisher = Elsevier Science Ltd.
| series = European Geothermal Conference 2003
| year = 2003
| issn = 0375-6505
| doi = 10.1016/S0375-6505(03)00053-1}}
</ref> The global average was 73% in 2005.


== Resources ==
== Resources ==

Revision as of 18:19, 14 June 2011

Part of a series on
Renewable energy

Geothermal electricity is electricity generated from geothermal energy. Technologies in use include dry steam power plants, flash steam power plants and binary cycle power plants. Geothermal electricity generation is currently used in 24 countries[1] while geothermal heating is in use in 70 countries.[2]

Estimates of the electricity generating potential of geothermal energy vary from 35 to 2000 GW.[2] Current worldwide installed capacity is 10,715 megawatts (MW), with the largest capacity in the United States (3,086 MW),[3] Philippines, and Indonesia.

Geothermal power is considered to be sustainable because the heat extraction is small compared with the Earth's heat content.[4] The emission intensity of existing geothermal electric plants is on average 122 kg of CO
2 per megawatt-hour (MW·h) of electricity, about one-eighth of a conventional coal-fired plant.[5]

History and development

Global geothermal electric capacity. Upper red line is installed capacity;[6] lower green line is realized production.[2]

In the 20th century, demand for electricity led to the consideration of geothermal power as a generating source. Prince Piero Ginori Conti tested the first geothermal power generator on 4 July 1904 in Larderello, Italy. It successfully lit four light bulbs.[7] Later, in 1911, the world's first commercial geothermal power plant was built there. Experimental generators were built in Beppu, Japan and the Geysers, California, in the 1920s, but Italy was the world's only industrial producer of geothermal electricity until 1958.

In 1958, New Zealand became the second major industrial producer of geothermal electricity when its Wairakei station was commissioned. Wairakei was the first plant to use flash steam technology.[8]

In 1960, Pacific Gas and Electric began operation of the first successful geothermal electric power plant in the United States at The Geysers in California.[9] The original turbine lasted for more than 30 years and produced 11 MW net power.[10]

The binary cycle power plant was first demonstrated in 1967 in Russia and later introduced to the USA in 1981,[9] following the 1970s energy crisis and significant changes in regulatory policies. This technology allows the use of much lower temperature resources than were previously recoverable. In 2006, a binary cycle plant in Chena Hot Springs, Alaska, came on-line, producing electricity frntil recently been built exclusively where high temperature geothermal resources are available near the surface. The development of binary cycle power plants and improvements in drilling and extraction technology may enable enhanced geothermal systems over a much greater geographical range.[11] Demonstration projects are operational in Landau-Pfalz, Germany, and Soultz-sous-Forêts, France, while an earlier effort in Basel, Switzerland was shut down after it triggered earthquakes. Other demonstration projects are under construction in Australia, the United Kingdom, and the United States of America.[12]

The thermal efficiency of geothermal electric plants is low, around 10-23%,[13] because geothermal fluids are at a low temperature compared with steam from boilers. By the laws of thermodynamics this low temperature limits the efficiency of heat engines in extracting useful energy during the generation of electricity. WOW!!!!!!!!!!!!!!!!!

Resources

Enhanced geothermal system 1:Reservoir 2:Pump house 3:Heat exchanger 4:Turbine hall 5:Production well 6:Injection well 7:Hot water to district heating 8:Porous sediments 9:Observation well 10:Crystalline bedrock

The earth’s heat content is 1031 joules.[2] This heat naturally flows to the surface by conduction at a rate of 44.2 terawatts, (TW,)[14] and is replenished by radioactive decay at a rate of 30 TW.[4] These power rates are more than double humanity’s current energy consumption from primary sources, but most of this power is too diffuse (approximately 0.1 W/m2 on average) to be recoverable. The Earth's crust effectively acts as a thick insulating blanket which must be pierced by fluid conduits (of magma, water or other) to release the heat underneath.

Electricity generation requires high temperature resources that can only come from deep underground. The heat must be carried to the surface by fluid circulation, either through magma conduits, hot springs, hydrothermal circulation, oil wells, drilled water wells, or a combination of these. This circulation sometimes exists naturally where the crust is thin: magma conduits bring heat close to the surface, and hot springs bring the heat to the surface. If no hot spring is available, a well must be drilled into a hot aquifer. Away from tectonic plate boundaries the geothermal gradient is 25-30°C per kilometre (km) of depth in most of the world, and wells would have to be several kilometres deep to permit electricity generation.[2] The quantity and quality of recoverable resources improves with drilling depth and proximity to tectonic plate boundaries.

In ground that is hot but dry, or where water pressure is inadequate, injected fluid can stimulate production. Developers bore two holes into a candidate site, and fracture the rock between them with explosives or high pressure water. Then they pump water or liquefied carbon dioxide down one borehole, and it comes up the other borehole as a gas.[11] This approach is called hot dry rock geothermal energy in Europe, or enhanced geothermal systems in North America. Much greater potential may be available from this approach than from conventional tapping of natural aquifers.[11]

Estimates of the electricity generating potential of geothermal energy vary from 35 to 2000 GW depending on the scale of investments.[2] This does not include non-electric heat recovered by co-generation, geothermal heat pumps and other direct use. A 2006 report by the Massachusetts Institute of Technology (MIT), that included the potential of enhanced geothermal systems, estimated that investing 1 billion US dollars in research and development over 15 years would allow the creation of 100 GW of electrical generating capacity by 2050 in the United States alone.[11] The MIT report estimated that over 200 zettajoules (ZJ) would be extractable, with the potential to increase this to over 2,000 ZJ with technology improvements - sufficient to provide all the world's present energy needs for several millennia.[11]

At present, geothermal wells are rarely more than 3 kilometres (2 mi) deep.[2] Upper estimates of geothermal resources assume wells as deep as 10 kilometres (6 mi). Drilling at this depth is now possible in the petroleum industry, although it is an expensive process. The deepest research well in the world, the Kola superdeep borehole, is 12 kilometres (7 mi) deep.[15] This record has recently been imitated by commercial oil wells, such as Exxon's Z-12 well in the Chayvo field, Sakhalin.[16] Wells drilled to depths greater than 4 kilometres (2 mi) generally incur drilling costs in the tens of millions of dollars.[17] The technological challenges are to drill wide bores at low cost and to break larger volumes of rock.

Geothermal power is considered to be sustainable because the heat extraction is small compared to the Earth's heat content, but extraction must still be monitored to avoid local depletion.[4] Although geothermal sites are capable of providing heat for many decades, individual wells may cool down or run out of water. The three oldest sites, at Larderello, Wairakei, and the Geysers have all reduced production from their peaks. It is not clear whether these plants extracted energy faster than it was replenished from greater depths, or whether the aquifers supplying them are being depleted. If production is reduced, and water is reinjected, these wells could theoretically recover their full potential. Such mitigation strategies have already been implemented at some sites. The long-term sustainability of geothermal energy has been demonstrated at the Lardarello field in Italy since 1913, at the Wairakei field in New Zealand since 1958,[18] and at The Geysers field in California since 1960.[19]

Power station types

File:Diagram-VaporDominatedGeothermal.jpg
Dry steam plant
File:Diagram-HotWaterGeothermal.jpg
Flash steam plant

Geothermal power stations are not dissimilar to other steam turbine thermal power stations - heat from a fuel source (in geothermal's case, the earth's core) is used to heat water or another working fluid. The working fluid is then used to turn a turbine, which in turn a generator to produce electricity. The fluid is then cooled and returned to the heat source.

Dry steam power plants

Dry steam plants are the simplest and oldest design. They directly use geothermal steam of 150°C or more to turn turbines.[2]

Flash steam power plants

Flash steam plants pull deep, high-pressure hot water into lower-pressure tanks and use the resulting flashed steam to drive turbines. They require fluid temperatures of at least 180°C, usually more. This is the most common type of plant in operation today.[20]

Binary cycle power plants

Main article: Binary cycle

Binary cycle power plants are the most recent development, and can accept fluid temperatures as low as 57°C.[21] The moderately hot geothermal water is passed by a secondary fluid with a much lower boiling point than water. This causes the secondary fluid to flash to vapor, which then drives the turbines. This is the most common type of geothermal electricity plant being built today.[22] Both Organic Rankine and Kalina cycles are used. The thermal efficiency of this type plant is typically about 10-13%.

Worldwide production

Larderello Geothermal Station, in Italy

The International Geothermal Association (IGA) has reported that 10,715 megawatts (MW) of geothermal power in 24 countries is online, which is expected to generate 67,246 GWh of electricity in 2010.[1] This represents a 20% increase in geothermal power online capacity since 2005. IGA projects this will grow to 18,500 MW by 2015, due to the large number of projects presently under consideration, often in areas previously assumed to have little exploitable resource.[1]

In 2010, the United States led the world in geothermal electricity production with 3,086 MW of installed capacity from 77 power plants;[3] the largest group of geothermal power plants in the world is located at The Geysers, a geothermal field in California.[23] The Philippines follows the US as the second highest producer of geothermal power in the world, with 1,904 MW of capacity online; geothermal power makes up approximately 18% of the country's electricity generation.[3]

January 2011: Al Gore said in The Climate Project Asia Pacific Summit that Indonesia could become a super power country in electricity production from geothermal energy.[24]

Utility-grade plants

The largest group of geothermal power plants in the world is located at The Geysers, a geothermal field in California, United States.[25] As of 2004, five countries (El Salvador, Kenya, the Philippines, Iceland, and Costa Rica) generate more than 15% of their electricity from geothermal sources.[2]

Naknek Electric Association (NEA) is going to make an exploration well near King Salmon, in Southwest Alaska. It could cut the cost of electricity production by 71 percent and the planned power is 25 megawatts.[26]

Geothermal electricity is generated in the 24 countries listed in the table below. During 2005, contracts were placed for an additional 500 MW of electrical capacity in the United States, while there were also plants under construction in 11 other countries.[11] Enhanced geothermal systems that are several kilometres in depth are operational in France and Germany and are being developed or evaluated in at least four other countries.

Installed geothermal electric capacity
Country Capacity (MW)
2007[6] 		Capacity (MW)
2010[27] 		percentage
of national
production
USA 2687 3086 0.3%
Philippines 1969.7 1904 27%
Indonesia 992 1197 3.7%
Mexico 953 958 3%
Italy 810.5 843
New Zealand 471.6 628 10%
Iceland 421.2 575 30%
Japan 535.2 536 0.1%
El Salvador 204.2 204 14%
Kenya 128.8 167 11.2%
Costa Rica 162.5 166 14%
Turkey 38 94 0.3%
Nicaragua 87.4 88 10%
Russia 79 82
Papua-New Guinea 56 56
Guatemala 53 52
Portugal 23 29
China 27.8 24
France 14.7 16
Ethiopia 7.3 7.3
Germany 8.4 6.6
Austria 1.1 1.4
Australia 0.2 1.1
Thailand 0.3 0.3
TOTAL 9,731.9 10,709.7

Environmental impact

Krafla Geothermal Station in northeast Iceland

Fluids drawn from the deep earth carry a mixture of gases, notably carbon dioxide (CO
2), hydrogen sulfide (H
2S), methane (CH
4), and ammonia (NH
3). These pollutants contribute to global warming, acid rain, and noxious smells if released. Existing geothermal electric plants emit an average of 122 kg of CO
2 per megawatt-hour (MW·h) of electricity, a small fraction of the emission intensity of conventional fossil fuel plants.[5] Plants that experience high levels of acids and volatile chemicals are usually equipped with emission-control systems to reduce the exhaust. Geothermal plants could theoretically inject these gases back into the earth, as a form of carbon capture and storage.

In addition to dissolved gases, hot water from geothermal sources may hold in solution trace amounts of toxic chemicals, such as mercury, arsenic, boron, antimony, and salt.[28] These chemicals come out of solution as the water cools, and can cause environmental damage if released. The modern practice of injecting geothermal fluids back into the Earth to stimulate production has the side benefit of reducing this environmental risk.

Plant construction can adversely affect land stability. Subsidence has occurred in the Wairakei field in New Zealand.[29] Enhanced geothermal systems can trigger earthquakes as part of hydraulic fracturing. The project in Basel, Switzerland was suspended because more than 10,000 seismic events measuring up to 3.4 on the Richter Scale occurred over the first 6 days of water injection.[30]

Geothermal has minimal land and freshwater requirements. Geothermal plants use 3.5 square kilometres per gigawatt of electrical production (not capacity) versus 32 and 12 square kilometres for coal facilities and wind farms respectively.[29] They use 20 litres of freshwater per MW·h versus over 1000 litres per MW·h for nuclear, coal, or oil.[29]

Economics

Geothermal power requires no fuel, and is therefore immune to fuel cost fluctuations, but capital costs tend to be high. Drilling accounts for over half the costs, and exploration of deep resources entails significant risks. A typical well doublet in Nevada can support 4.5 megawatt (MW) of electricity generation and costs about $10 million to drill, with a 20% failure rate.[17] In total, electrical plant construction and well drilling cost about 2-5 million € per MW of electrical capacity, while the levelised energy cost is 0.04-0.10 € per kW·h.[6] Enhanced geothermal systems tend to be on the high side of these ranges, with capital costs above $4 million per MW and levelized costs above $0.054 per kW·h in 2007.[31]

Geothermal power is highly scalable: a large geothermal plant can power entire cities while a smaller power plant can supply a rural village.[32]

Chevron Corporation is the world's largest private producer of geothermal electricity.[33] The most developed geothermal field is the Geysers in California. In 2008, this field supported 15 plants, all owned by Calpine, with a total generating capacity of 725 MW.[25]

References

  1. ^ a b c Geothermal Energy Association. Geothermal Energy: International Market Update May 2010, p. 4-6.
  2. ^ a b c d e f g h i Fridleifsson,, Ingvar B.; Bertani, Ruggero; Huenges, Ernst; Lund, John W.; Ragnarsson, Arni; Rybach, Ladislaus (2008-02-11), O. Hohmeyer and T. Trittin (ed.), The possible role and contribution of geothermal energy to the mitigation of climate change (pdf), Luebeck, Germany, pp. 59–80, retrieved 2009-04-06 {{citation}}: Unknown parameter |conference= ignored (help)CS1 maint: extra punctuation (link) CS1 maint: location missing publisher (link)
  3. ^ a b c Geothermal Energy Association. Geothermal Energy: International Market Update May 2010, p. 7.
  4. ^ a b c Rybach, Ladislaus (September 2007), "Geothermal Sustainability" (PDF), Geo-Heat Centre Quarterly Bulletin, vol. 28, no. 3, Klamath Falls, Oregon: Oregon Institute of Technology, pp. 2–7, ISSN 0276-1084, retrieved 2009-05-09
  5. ^ a b Bertani, Ruggero; Thain, Ian (July 2002), "Geothermal Power Generating Plant CO2 Emission Survey" (PDF), IGA News (49), International Geothermal Association: 1–3, retrieved 2009-05-13
  6. ^ a b c Bertani, Ruggero (September 2007), "World Geothermal Generation in 2007" (PDF), Geo-Heat Centre Quarterly Bulletin, vol. 28, no. 3, Klamath Falls, Oregon: Oregon Institute of Technology, pp. 8–19, ISSN 0276-1084, retrieved 2009-04-12
  7. ^ Tiwari, G. N.; Ghosal, M. K. Renewable Energy Resources: Basic Principles and Applications. Alpha Science Int'l Ltd., 2005 ISBN 1842651250
  8. ^ http://www.ipenz.org.nz/heritage/itemdetail.cfm?itemid=84
  9. ^ a b Lund, J. (September 2004), "100 Years of Geothermal Power Production" (PDF), Geo-Heat Centre Quarterly Bulletin, vol. 25, no. 3, Klamath Falls, Oregon: Oregon Institute of Technology, pp. 11–19, ISSN 0276-1084, retrieved 2009-04-13
  10. ^ McLarty, Lynn; Reed, Marshall J. (October 1992), "The U.S. Geothermal Industry: Three Decades of Growth" (PDF), Energy Sources, Part A: Recovery, Utilization, and Environmental Effects, 14 (4), London: Taylor & Francis: 443–455, doi:10.1080/00908319208908739, ISSN 1556-7230
  11. ^ a b c d e f Tester, Jefferson W. (Massachusetts Institute of Technology); et al., The Future of Geothermal Energy (14MB PDF), Impact, vol. of Enhanced Geothermal Systems (Egs) on the United States in the 21st Century: An Assessment, Idaho Falls: Idaho National Laboratory, ISBN 0-615-13438-6, retrieved 2007-02-07 {{citation}}: Explicit use of et al. in: |first= (help)
  12. ^ Bertani, Ruggero (2009), "Geothermal Energy: An Overview on Resources and Potential" (PDF), Proceedings of the International Conference on National Development of Geothermal Energy Use, Slovakia {{citation}}: Missing or empty |title= (help)CS1 maint: location missing publisher (link)
  13. ^ http://gafoen.com/site/index.php?page=geothermalenergy
  14. ^ Pollack, H.N. (1993), "Heat Flow from the Earth's Interior: Analysis of the Global Data Set", Rev. Geophys., vol. 30, no. 3, pp. 267–280 {{citation}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  15. ^ Cassino, Adam (2003). "Depth of the Deepest Drilling". The Physics Factbook. Glenn Elert. Retrieved 2009-04-09.
  16. ^ Watkins, Eric (February 11, 2008), "ExxonMobil drills record extended-reach well at Sakhalin-1", Oil & Gas Journal, retrieved 2009-10-31
  17. ^ a b Geothermal Economics 101, Economics of a 35 MW Binary Cycle Geothermal Plant, New York: Glacier Partners, October 2009, retrieved 2009-10-17
  18. ^ Thain, Ian A. (September 1998), "A Brief History of the Wairakei Geothermal Power Project" (PDF), Geo-Heat Centre Quarterly Bulletin, vol. 19, no. 3, Klamath Falls, Oregon: Oregon Institute of Technology, pp. 1–4, ISSN 0276-1084, retrieved 2009-06-02
  19. ^ Axelsson, Gudni; Stefánsson, Valgardur; Björnsson, Grímur; Liu, Jiurong (April 2005), "Sustainable Management of Geothermal Resources and Utilization for 100 – 300 Years" (PDF), Proceedings World Geothermal Congress 2005, International Geothermal Association, retrieved 2009-06-02
  20. ^ US DOE EERE Hydrothermal Power Systems
  21. ^ Erkan, K.; Holdmann, G.; Benoit, W.; Blackwell, D. (2008), "Understanding the Chena Hot Springs, Alaska, geothermal system using temperature and pressure data", Geothermics, 37 (6): 565–585, doi:10.1016/j.geothermics.2008.09.001, ISSN 0375-6505, retrieved 2009-04-11
  22. ^ "Geothermal Basics Overview". Office of Energy Efficiency and Renewable Energy. Retrieved 2008-10-01.
  23. ^ Khan, M. Ali (2007), The Geysers Geothermal Field, an Injection Success Story (pdf), Annual Forum of the Groundwater Protection Council, retrieved 2010-01-25
  24. ^ http://www.antaranews.com/en/news/1294577958/indonesia-can-be-super-power-on-geothermal-energy-al-gore
  25. ^ a b "Calpine Corporation (CPN) (NYSE Arca) Profile" (Press release). Reuters. Retrieved 2009-10-14.
  26. ^ http://www.renewableenergyworld.com/rea/news/article/2009/05/naknek-electric-utility-heats-up-geothermal-plans?cmpid=WNL-Wednesday-May6-2009
  27. ^ Holm, Alison (May 2010), Geothermal Energy:International Market Update (PDF), Geothermal Energy Association, p. 7, retrieved 2010-05-24
  28. ^ Bargagli1, R.; Catenil, D.; Nellil, L.; Olmastronil, S.; Zagarese, B. (August 1997), "Environmental Impact of Trace Element Emissions from Geothermal Power Plants", Environmental Contamination Toxicology, 33 (2), New York: Springer: 172–181, doi:10.1007/s002449900239, ISSN 0090-4341{{citation}}: CS1 maint: numeric names: authors list (link)
  29. ^ a b c Lund, John W. (June 2007), "Characteristics, Development and utilization of geothermal resources" (PDF), Geo-Heat Centre Quarterly Bulletin, vol. 28, no. 2, Klamath Falls, Oregon: Oregon Institute of Technology, pp. 1–9, ISSN 0276-1084, retrieved 2009-04-16
  30. ^ Deichmann, N.; et al. (2007), Seismicity Induced by Water Injection for Geothermal Reservoir Stimulation 5 km Below the City of Basel, Switzerland, American Geophysical Union, Bibcode:2007AGUFM.V53F..08D {{citation}}: Explicit use of et al. in: |first= (help)
  31. ^ Sanyal, Subir K.; Morrow, James W.; Butler, Steven J.; Robertson-Tait, Ann (January 22–24, 2007), "Cost of Electricity from Enhanced Geothermal Systems" (PDF), Proc. Thirty-Second Workshop on Geothermal Reservoir Engineering, Stanford, California {{citation}}: Missing or empty |title= (help)CS1 maint: location missing publisher (link)
  32. ^ Lund, John W.; Boyd, Tonya (June 1999), "Small Geothermal Power Project Examples" (PDF), Geo-Heat Centre Quarterly Bulletin, vol. 20, no. 2, Klamath Falls, Oregon: Oregon Institute of Technology, pp. 9–26, ISSN 0276-1084, retrieved 2009-06-02
  33. ^ Davies, Ed; Lema, Karen (June 29, 2008), "Pricey oil makes geothermal projects more attractive for Indonesia and the Philippines", The New York Times, retrieved 2009-10-31
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