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Geothermal Energy

Geothermal Energy

The word "geothermal" is derived from the Greek words geo (earth) and therme (heat), and "energy" is defined as usable power, such as heat or electricity. The temperature at the Earth's core (6,437 kilometers or 4,000 miles deep) may exceed 4,980°C (9,000°F). Energy from the Earth's interior, in the form of heat, constantly flows outward. Upwelling of hot mantle material to shallower depths and lower pressure produces melting, forming a magma (molten rock) that is less dense than the mantle material from which it was derived. This less dense magma rises slowly through the mantle to the Earth's crust. If the magma reaches the Earth's surface, it is called lava.

If magma remains beneath the Earth's surface within the crust, the heat energy is released slowly over time to the local and even regional area. This residual heat energy transfers to adjacent rock and groundwater , heating them to temperatures exceeding 370°C (700°F). Most of this heat energy remains stored in the Earth's depths, creating geothermal reservoirs. Some heat energy from the geothermal reservoirs transfers to deep-circulating groundwater, and the superheated water travels to the Earth's surface via faults and fractures, creating geysers and hot springs .

High-temperature geothermal resources (temperatures greater than 150°C, or 302°F) are primarily found in volcanic regions and island chains, whereas low-temperature geothermal resources (temperatures less than 100°C, or 212°F) are found throughout the world and on all continents. Worldwide, high-temperature resources usually are found in tectonic settings associated with volcanism , such as the Pacific Rim (the so-called "Ring of Fire")* and in Iceland. In the United States, energy use associated with geothermal reservoirs takes place primarily in the western states and Hawaii, which are areas of geologically recent volcanism.

Using Geothermal Energy

From prehistoric times, humans have utilized the geothermal energy that flows freely from underground reservoirs to the Earth's surface. The Romans used geothermal water to treat various diseases as well as to heat the city of Pompeii. Native North Americans used geothermal water for cooking and medicinal purposes for more than 10,000 years, and the Maoris of New Zealand have cooked geothermally for centuries. Ancient records in Iceland mention the use of geothermal springs for washing and bathing.

Today, geothermal energy is utilized in three technology categories:

  • Heating and cooling buildings via geothermal heat pumps that utilize shallow sources;
  • Heating structures with direct-use applications; and
  • Generating electricity through indirect use.

Heat Pumps.

Most areas of the world are suitable for geothermal heat pumps; hence, there is a great potential for future worldwide use of heat-pump technology. Geothermal heat pumps take advantage of the fact that a majority of the Earth's upper 3 meters (less than 10 feet) maintain temperatures ranging from 10 to 15.5°C (50 to 60°F).

A geothermal pump system consists of pipes buried horizontally in the upper 3 meters adjacent to a building and then tied into the structure's ventilation system by simply using the subsurface as a heat exchanger. A liquid passed through the pipes picks up residual underground heat in winter, then delivers it to the building, thus warming it. In summer, the liquid transfers heat from the building to the ground, thus cooling the building.

Direct Use.

Direct-use applications utilize groundwater that has been heated to generally less than 100°C (212°F). Direct use of geothermal energy can supply heat for industrial processes, and can boost agricultural and aquaculture production in cold climates by heating greenhouses, soils, and aquaculture ponds. Geothermal uses also include hot spring and spa bathing, as well as residential and regional (district) heating.

Direct uses annually provide 11,000 thermal megawatts of power worldwide. In Reykjavik, Iceland, more than 95 percent of the buildings are heated with geothermal water pumped from deep wells. The city of Klamath Falls, Oregon (USA) heats 35 percent of all residential dwellings and also heats most downtown sidewalks in the winter.

Electricity Generation.

High-temperature geothermal resources almost always are used for power production. Although geothermal energy has been used throughout history, the indirect generation of electricity is relatively new. Wells are drilled into known geothermal reservoirs where temperatures often exceed 360°C (680°F). Steam or super-heated water is brought to the surface under its own pressure where the energy, in the form of steam, is utilized to turn the turbines of an electrical generator.

Three types of geothermal power plants are operating today:

  • Dry steam plants, which directly use geothermal steam to turn turbines;
  • Flash steam plants, which pull deep, high-pressure hot water into lower-pressure tanks and use the resulting flashed steam to drive turbines; and
  • Binary-cycle plants, which pass (in separate piping) moderately hot geothermal water by a secondary fluid with a much lower boiling point than water. This causes the secondary fluid to flash to steam, which then drives the turbines.

Geothermal electric power generation is a proven technology that is significant in nations with no indigenous fossil fuel resources. Moreover, it is a renewable energy source and one that is considered cleaner than fossil fuel (e.g., geothermal power plants emit less carbon dioxide). Worldwide, geothermal energy produced 7,500 megawatts in 21 countries (mostly developing) in 2000, serving 60 million people. The United States produced 3,000 megawatts from geothermal power plants, supplying about 4 million people.

Environmental Considerations.

Comparatively speaking, geothermal energy is more "environmentally friendly" than fossil fuels or nuclear fission. However, emissions of carbon dioxide gas and smaller amounts of hydrogen sulfide accompany the geothermal fluids extracted from wells. Moreover, hot brine liberated by drilling must be carefully managed to prevent environmental damage and potential human health impacts.

To prevent ground subsidence (sinking) caused by the extraction of geothermal fluids from their underground reserves, waste brines often are reinjected into the well. Reinjection must be done carefully to avoid contaminating potable (drinkable) groundwater supplies. Above-ground disposal of waste brine also must be managed to avoid contamination of seas and waterways.

As more geothermal resources are exploited for their electricity-producing capabilities, it will become increasingly important to control carbon dioxide emissions and properly manage waste brines and other byproducts of mining and power production.

see also Earth's Interior, Water in the; Fresh Water, Natural Composition of; Fresh Water, Physics and Chemistry of; Groundwater; Hot Springs and Geysers; Mineral Water and Spas; Plate Tectonics; Springs; Volcanoes and Water.

Rick G. Graff

Bibliography

Putnam, William Clement. Putnam's Geology, 5th ed. New York: Oxford University Press, 1997.

Duffield, W. A., J. H. Sass, and M. L. Sorey. Tapping the Earth's Natural Heat. U.S. Geological Survey Circular 1125 (1994).

Harsh, Gupta K. Geothermal Resources: An Energy Alternative. New York: Elsevier, 1980.

Internet Resources

Geo-Heat Center. Oregon Institute of Technology. <http://geoheat.oit.edu>.

Geothermal Education Office. <http://www.geothermal.marin.org>.

Geothermal Energy. The World Bank Group. <http://www.worldbank.org/html/fpd/energy/geothermal>.

Geothermal Resources in Iceland. District Energy Library, University of Rochester. <http://www.energy.rochester.edu/is/reyk>.

Soulsby, David. North Atlantic Hot Spot: A Geological History of Iceland. Kibo Productions Ltd. <http://www.kibo-productions.co.uk/nahscript.htm>.

FIRST GEOTHERMAL PLANTS

The first power plant to utilize a geothermal well was brought online in Larderello, Italy in 1904. The first geothermal plant in the United States was at The Geysers in Northern California in 1962.

These two geothermal fields are unusual because they emit dry steam, which is superheated steam with no associated fluids. This kind of steam is preferred over wet steam (the more common kind of steam found in geothermal fields) because it contains less corroding elements and less waste to deal with.

* See "Volcanoes, Submarine" for an illustration showing the Ring of Fire's location.

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Geothermal Energy

Geothermal energy

The discovery that the temperature in deep mines exceeded the surface temperature implied the existence of a source of deep geothermal energy. Within the continental crusts, the temperature differential gradient averages about one micro calorie per square centimeter (equivalent to an increase of about 95°F per mile or 33°C per kilometer of increasing depth).

In some areas geothermal energy is a viable economic alternative to conventional energy generation. Commercially viable geothermal fields have the same basic structure. The source of heat is generally a magmatic intrusion into Earth's crust . The magma intrusion generally measures 11101650°F (600900°C), at a depth of 4.39.3 mi (715 km). The bedrock containing the intrusion conducts heat to overlying aquifers (i.e., layers of porous rock such as sandstone that contain significant amounts of water ) covered by a dome-shaped layer of impermeable rock such as shale or by an over-lying fault thrust that contains the heated water and/or steam. A productive geothermal generally produces about 20 tons (18.1 metric tons) of steam, or several hundred tons of hot water, per hour. Historically, some heavily exploited geothermal fields have had decreasing yields due to a lack of replenishing water in the aquifer , rather than to cooling of the bedrock.

There are three general types of geothermal fields: hot water, wet steam, and dry steam. Hot water fields contain reservoirs of water with temperatures between 140212°F (60100°C), and are most suitable for space heating and agricultural applications. For hot water fields to be commercially viable, they must contain a large amount of water with a temperature of at least 140°F (60°C) and lie within 2,000 meters of the surface.

Wet steam fields contain water under pressure and usually measure 212°F (100°C). These are the most common commercially exploitable fields. When the water is brought to the surface, some of the water flashes into steam, and the steam may drive turbines that can produce electrical power.

Dry steam fields are geologically similar to wet steam fields, except that superheated steam is extracted from the aquifer. Dry steam fields are relatively uncommon.

Because superheated water explosively transforms into steam when exposed to the atmosphere, it is much safer and generally more economical to use geothermal energy to generate electricity , which is much more easily transported. Because of the relatively low temperature of the steam/water, geothermal energy may be converted into electricity with an efficiency of 1015%, as opposed to 2025% for coal or oil fired generated electricity.

To be commercially viable, geothermal electrical generation plants must be located near a large source of easily accessible geothermal energy. A further complication in the practical utilization of geothermal energy derives from the corrosive properties of most groundwater and steam. In fact, prior to 1950, metallurgy was not advanced enough to enable the manufacture of steam turbine blades resistant to corrosion . Geothermal energy sources for space heating and agriculture have been used extensively in Iceland, and to some degree Japan, New Zealand, and the former Soviet Union. Other applications include paper manufacturing and water desalination .

While geothermal energy is generally presented as nonpolluting energy source, water from geothermal fields often contains large amounts of hydrogen sulfide and dissolved metals , making its disposal difficult.

See also Earth, interior structure; Energy transformations; Geothermal deep ocean vents; Geothermal gradient; Temperature and temperature scales

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geothermal energy

geothermal energy Heat contained in the Earth's crust. It is produced by radioactivity within the Earth's core and by the movement of tectonic plates. It is released naturally by geysers, volcanoes and hot springs, and can be used as a power source for generating electricity. See also plate tectonics; volcano

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geothermal energy

geothermal energy: see energy, sources of.

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