The Earth's crust,
on which we live and depend, is in large part the product of
millions of once-active volcanoes and tremendous volumes of magma that
did not erupt but instead cooled below the surface. Such
persistent and widespread volcanism has resulted in many valuable
natural
resources throughout the world. ...
Groundwater heated by
large, still-hot magma bodies can be tapped for geothermal energy.
-- Excerpt from:
Brantley, 1994, Volcanoes of the United States, USGS General
Interest Publication
In general
there are two main categories, (1)
the high temperature resources and (2)
the moderate/low temperature resources. The high temperature geothermal
resources - 220 degrees Celsius and up - are predominantly found in
volcanic regions and island chains. The moderate to low temperature
resources are found on all continents. The high temperature are almost
always used for power production while most of the low temperature
resources are used for direct heating purposes or agriculture and
aquaculture.
How does Harnessing
Geothermal Energy Work?
Deep
wells, a mile or more deep, can tap reservoirs of steam or very hot
water that can be used to drive turbines which power electricity
generators.
There are
3 types of geothermal power plants in use today, and they are:
Dry Steam
Plants
which use geothermal steam directly. Dry steam power plants use very
hot (>455 °F, or >235 °C) steam
and little water from the geothermal reservoir. The steam
goes directly through a pipe to a turbine to spin a generator that
produces electricity. This type of geothermal power plant is the
oldest, first being used at Lardarello, Italy, in 1904. An example of a dry
steam generation operation is at the Geysers in North California, shown
at right
(Green Jobs, 2002).
Flash Steam Plants which use high pressure hot water to
produce steam when thepressure is reduced. Flash steam power plants use
hot water (>360 ºF, or >182 ºC) from the geothermal
reservoir. When the water is pumped to the generator, it is released
from the pressure of the deep reservoir. The sudden drop in pressure
causes some of the water to vaporize to steam, which spins a turbine to
generate electricity. Both dry steam and flash steam power plants emit
small amounts of carbon dioxide, nitric oxide, and sulfur, but
generally 50 times less than traditional fossil-fuel power plants.16
Hot water not flashed into steam is returned to the geothermal
reservoir through injection wells (Green Jobs, 2002).
Binary Cycle Plants
which use moderate-temperature water (225 to 360 ºF, or 107 to 182
ºC) from the geothermal reservoir. In binary systems, hot
geothermal fluids are passed through one side of a heat exchanger to
heat a working fluid in a separate adjacent pipe. The working fluid,
usually an organic compound with a low boiling point such as Iso-butane
or Iso-pentane, is vaporized and passed through a turbine to generate
electricity. An ammonia-water working fluid is also used in what is
known as the Kalina Cycle. Makers claim that the Kalina Cycle system
boosts geothermal plant efficiency by 20-40% and reduces plant
construction costs by 20-30%, thereby lowering the cost of geothermal
power generation (Green Jobs, 2002). The Mammoth Pacific binary
geothermal power plant, located at the Casa Diablo geothermal field, is
pictured at right (Idaho National Engineering and Environmental
Laboratory, 2004).
There is also
another method, called
geothermal heat pumps. The
earth’s surface layer remains at an almost constant temperature between
10 to 16C (50 to 50F). In this method, geothermal heat pumps use a
system of buried
pipes linked to a heat exchanger and ductwork into buildings. In winter
the relatively warm earth transfers heat into the buildings and in
summer the buildings transfer heat to the ground or uses some of it to
heat water. These heat pumps function as both air-conditioning and
heating systems in one (Green Jobs, 2002)
U.S. Geothermal
Energy Potential
In 1999, geothermal energy provided 0.4%
of
U.S. electricity generation (14.3 billion kWh), enough to supply
electricity to over 1,400,000 average
U.S. homes. U.S. geothermal
capacity grew only slightly from 1990 to 1998, by 2.7% from 2,775 MW to
2,850 MW. Worldwide, geothermal capacity in 1999 was 8.24 million kW,
or 0.26% of the 3,180 million kW of total world installed electrical
generating capacity. Worldwide geothermal capacity grew much more
rapidly than the U.S. over the last decade, by over 40% from 5,867 MW
in 1990 to 8,240 MW in 1998. However, the United States still accounted
for 35% of worldwide installed geothermal capacity in 1998 (Geothermal
Education Office, 2003).
Puna Geothermal, the only geothermal power plant in Hawaii, can
generate a net of 25 MW of electrical energy (or 24% of Hawaii's
electrical energy) from the geothermal fluids produced from the Puna
geothermal field (USGS, 2004).
Applications of
Geothermal Energy
1.
Space/District Heating: Schemes utilizing
geothermal heat
provide over 80% of the central heating needs of Reykjavik city in
Iceland and are employed in many towns in USA, Poland and Hungary. The
World Bank is currently supporting a program in Poland for using hot
water from unsuccessful oil wells to displace the use of coal for
district heating (World Bank Group, 2004).
2.
Agriculture and Aquaculture: In temperate and
colder climates, greatly improved plant and fish growth can be achieved
by heating soils, greenhouses and fish ponds using geothermal heat. One
example of this is the largely successful Osearian Farm, Kenya (World
Flowers, 2005).
3. Power
Generation: With over 8000 MW
of installed
capacity, geothermal electric power generation is a well-proven
technology that has been especially successful in countries and islands
that have a high reliance on imported fossil fuels (World Bank Group,
2004).
Costs of Geothermal
Energy
Costs
for geothermal electricity generation are 4.5-7 cents per
kilowatt-hour. This is competitive with some fossil fuel facilities,
but one must keep in mind the drastic reduction of pollution. Delivered
costs depend on ownership arrangements, financing, transmission, the
quality of the resource, and the size of the project.
Geothermal plants are relatively capital-intensive, with low variable
costs and no fuel costs. Usually financing is structured so that the
project pays back its capital costs in the first 15 years, delivering
power at 5-10¢/kWh. Costs then fall by 50-70 percent, to cover
just operations and maintenance for the remaining 15-30 years that the
facility operates (World Bank Group, 2004).
Other Benefits of
Geothermal Energy
1.
Minimize air pollution: Current
geothermal fields produce only about one-sixth of the carbon dioxide
that a natural gas fueled electrical generating power plant produces
and none of the nitrous oxide (NOx) or sulfur bearing (SOx) gases.
New state of the art geothermal binary and combined cycle plants
produce virtually no air emissions. Each 1,000 MW of new geothermal
power will offset 1.9 million pounds per year of noxious and toxic air
pollution emissions in Western skies and offset about 7.8 billion
pounds per year of climate affecting CO2 emissions from gas fired
plants or much larger amounts from coal fired plants (USGS, 2004).
2. Renewable energy source: All
types of geothermal energy are renewable as long as the rate of
heat extraction from the earth does not exceed the rate at which the
thermal reservoir it depends upon is recharged by the earthâs
heat. A
geothermal reservoir that has been used for electricity generation may
take several hundred years to recharge after it has been completely
depleted. District heating system reservoir recovery may take 100-200
years, and geothermal heat pump reservoir recovery may take30 years or
so.
3. Reduces dependence on imported
energy: Geothermal energy is generated with indigenous
resouces, thereby reducing trade deficits. Reducting trade deficits
keeps wealth at home and promotes healthier economies. Nearly half of
the U.S. annual trade deficit would be erased if imported oil were
displaces with domestic energy resources (Green Jobs, 2004).
Although
geothermal energy has been around for over a century, we are just now
realizing its potential for replacing and/or supplementing current
energy resources. In the U.S., most geothermal sources are in the
western states, including Alaska and Hawaii. This limited usage
seems to be geothermal energy's greatest downfall, despite being clean,
efficient, and cheap. When compared to other alternative
energies, such as solar, geothermal energy only outputs a small
fraction of that of solar energy dispersed atop the earth's
surface. We should consider its margin for improvement.
Although geothermal energy units can be expanded as needed, its methods
and its technologies have been virtually stagnant. Also, as we
explore alternative energy sources, we should consider its
appropriateness for various points on the globe.
Works Cited
nGeothermal
Education Office. “About Geothermal Energy.” 07 April 2003.
http://geothermal.marin.org/GEOpresentation/sld108.html
Green Jobs,
"Introduction to Geothermal Energy." 18 August, 2002.
http://www.greenjobs.com/Public/info/industry_background.aspx?id=11
n
U.S. Geological Survey. “The Plus Side of Volcanoes – Geothermal
Energy.” 16 December 2004.
http://vulcan.wr.usgs.gov/LivingWith/PlusSide/geothermal.html
n
World Flowers. “Technical: The Harnessing of Geothermal Energy.” 27
February 2005.
http://www.world-flowers.co.uk/09technical/geothermal.html