RENWABLE ENERGY INFORMATION HUB- Geothermal Energy
Oct 6, 07
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Geothermal Energy – A Viable Source |
Geothermal Power Technology
Utility-scale
geothermal power production employs three main technologies. These are known
as dry steam, flash steam and binary cycle systems. The technology employed
depends on the temperature and pressure of the geothermal reservoir. Unlike
solar, wind, and hydro-based renewable power, geothermal power plant
operation is independent of fluctuations in daily and seasonal weather.
Dry steam
Dry steam power plants use very hot (>455 °F, or >235 °C) steam and
little water from the geothermal reservoir.12 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 1904.13
Figure 2 is a schematic of a typical dry steam power plant.14
Flash steam
Flash steam power plants use hot water (>360 ºF, or >182 ºC) from the
geothermal reservoir.15 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. Figure 3 is a schematic of a typical flash steam power
plant.17

Binary-cycle
Binary-cycle power plants use moderate-temperature water (225 ºF–360 ºF, or
107 ºC–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 percent and reduces plant construction costs by
20–30 percent, thereby lowering the cost of geothermal power generation.
The advantages of binary cycle systems are that the working fluid boils at a lower temperature than water does, so electricity can be generated from reservoirs with lower temperature, and the binary cycle system is self-contained and therefore, produces virtually no emissions. For these reasons, some geothermal experts believe binary cycle systems could be the dominant geothermal power plants of the future. Figure 4 is a schematic of a typical binary cycle power plant.18

Economics
The commercial
viability of geothermal power production is influenced by capital costs for
land, drilling, and physical plant; operating and maintenance costs; the
amount of power generated and sold from the plant; and the market value of
that power. However, because geothermal power plants incur high capital costs
at the beginning of the project, they are typically at an economic
disadvantage to conventional fossil fueled power plants. Fossil fuel plants
have lower up-front capital costs, but incur fuel costs for the life of the
plant. This section discusses capital cost, operating and maintenance cost,
average cost of power production over the life of the plant (known as the
levelized cost of power production), as well as the
economic impacts of geothermal power such as labor creation, tax base
contributions, and balance-of-trade impacts.
Capital Cost Geothermal power plant
operating and maintenance costs range from $0.015 to $0.045 per KWh,
depending on how often the plant runs. Geothermal plants typically run 90% of
the time. They can be run up to 97–98% of the time, but this increases
maintenance costs. High run times are found when contractual agreements pay
high prices for power. Higher-priced electricity justifies running the plant
at high-capacity factors because the resulting higher maintenance costs are
recovered. Table 5 provides geothermal operating and maintenance cost by
plant size. Large plants tend to have lower O&M costs due to economies of
scale.
Cost Component
Small Plants
Medium Plants (5–30 MW)
Large Plants
Steam field
0.35–0.7
0.25–0.35
0.15–0.25
Power plants
0.45–0.7
0.35–0.45
0.25–0.45
Total
0.8–1.4
0.6–0.8
0.4–0.7
Resource
O&M Cost (cents/kWh)
Geothermal
0.4–1.4
Hydropower31
0.7
Coal32
0.46
Nuclear33
1.9
Levelized Cost
Real levelized costs for geothermal electricity generation are
$0.045-$0.07 per KWh, which is competitive with some fossil fuel facilities,
without the pollution.34 The lowest cost of geothermal electricity
is approximately $0.015 per KWh. At the Geysers, power is sold at $0.03 to
$0.035 per KWh. Some geothermal power plants can charge more per KWh during
some time periods, because of incentives related to reliability of generation
and power provided during peak demand. The cost of generating power from
geothermal resources has decreased about 25% over the past two decades.35
The goal of the
geothermal industry and the U.S. Department of Energy is to achieve a
geothermal energy life-cycle cost of electricity of $0.03 per KWh. It is
anticipated that costs in this range will result in about 10,000 MW of new
capacity installed by U.S. firms within the next decade. Table 7 presents the
levelized cost comparison of power by source. It
shows that in some cases, geothermal energy can compete directly with
conventional baseload power sources.
Table 7.
Levelized Cost Comparison
Resource
Levelized Cost36
Geothermal
1.5–7.0
Hydropower
0.5–2.4
Coal
2.0–5.0
Nuclear
1.5–3.0
Job Creation
Power Source
Construction
Employment (jobs/MW)
O&M Employment
(jobs/MW)
Total Employment for
500 MW Capacity
Factor Increase over
Natural Gas Wind 2.6 0.3 5,635 2.3 Geothermal 4.0 1.7 27,050 11.0 Solar PV 7.1 0.1 5,370 Solar
themal 5.7 0.2 6,155 2.5 Landfill
methan/digester gas 3.7 2.3 36,055 14.7 Natural gas 1.0 0.1 2,460 1.0
Geothermal energy
production in the United States is a $1.5-billion-dollar-per-year industry.40
Nevada’s geothermal plants produce about 210 MW of electricity, saving energy
imports equivalent to 800,000 tons of coal or 3 million barrels of oil each
year. In addition, state governments receive tax revenue. In 1993, Nevada’s
geothermal power plants paid $800,000 in county taxes and $1.7 million in
property taxes. The U.S. Bureau of Land Management collects nearly $20
million each year in rent and royalties from geothermal plants producing
power on federal lands in Nevada—half of these revenues are returned to the
state.41
Economic Impacts in Developing Countries
Developing countries
will likely require increasing amounts of power in the coming years. Through
technology transfer programs, some industrialized countries are helping
developing countries make use of their local sustainable and reliable
geothermal energy resources. Summary Our
intention has been to provide the reader with a balanced overview of the
utility-scale geothermal power industry. We believe clean, reliable power can
be developed from renewable resources, with geothermal power making an
important contribution. Examples from the U.S. geothermal sector have been
used to illustrate the costs, benefits, policies, and trends in geothermal
energy today. What follows is a list or further resources available on the
world-wide web to allow the reader to gain a deeper understanding of the
potential of geothermal power and the issues surrounding its development. We
urge the reader to seek further understanding of these issues, and the means
to their resolution, in order to support the progress of geothermal energy in
providing clean, reliable, and economic power. Geothermal Resources
Figure 1. Schematic of
geothermal power plant production and injection wells. Understanding
geothermal energy begins with an understanding of the source of this
energy—the earth’s internal heat. The Earth’s temperature increases with
depth, with the temperature at the center reaching more than 4200 °C (7600
°F). A portion of this heat is a relic of the planet’s formation about 4.5
billion years ago, and a portion is generated by the continuing decay of
radioactive isotopes. Heat naturally moves from hotter to cooler regions, so
Earth’s heat flows from its interior toward the surface.2 However, most magma remains below earth’s
crust and heats the surrounding rocks and subterranean water. Some of this
water comes all the way up to the surface through faults and cracks in the
earth as
hot springs
or geysers.
When this rising hot water and steam is trapped in permeable rocks under a
layer of impermeable rocks, it is called a
geothermal
reservoir. These reservoirs are sources of geothermal energy that
can potentially be tapped for electricity generation or direct use. Figure 1
is a schematic of a typical geothermal power plant showing the location of
magma and a geothermal reservoir.4 Here, the production well
withdraws heated geothermal fluid, and the injection well returns cooled
fluids to the reservoir. Geological,
hydrogeological, geophysical, and geochemical
techniques are used to identify and quantify geothermal resources. Geological and
hydrogeological
studies involve mapping any hot springs or other surface thermal features and
the identification of favorable geological structures. These studies are used
to recommend where production wells can be drilled with the highest
probability of tapping into the geothermal resource. Geophysical surveys
are implemented to figure the shape, size, depth and other important
characteristics of the deep geological structures by using the following
parameters: temperature (thermal survey), electrical conductivity (electrical
and electromagnetic methods), propagation velocity of elastic waves (seismic
survey), density (gravity survey), and magnetic susceptibility (magnetic
survey).5
Geochemical
surveys (including isotope geochemistry) are a useful means of
determining whether the geothermal system is water or vapor-dominated, of
estimating the minimum temperature expected at depth, of estimating the
homogeneity of the water supply and, of determining the source of recharge
water. Geothermal
exploration addresses at least nine objectives:6 Drilling
U.S.
Government Programs U.S.
Department of Energy
Capital costs are the fixed costs for power plant construction. Geothermal
capital costs include the cost of land, drilling of exploratory and steam
field wells, and physical plant, including buildings and power-generating
turbines. Geothermal plants are relatively capital-intensive, with low
variable costs and no fuel costs. The capital cost for geothermal power
plants ranges from $1150 to $3000 per installed KW, depending on the resource
temperature, chemistry, and technology employed. These costs may decrease
over time with additional technology development. Plant lifetimes are
typically 30–45 years. Financing is often structured such that the project
pays back its capital costs in the first 15 years. Costs then fall by 50–70%,
to cover just operations and maintenance for the remaining 15–30 years that
the facility operates.25 Table 3 shows the capital costs for
geothermal plants, and Table 4 shows conventional
baseload
power direct capital costs for comparison.
Table 4. Conventional Baseload Power Direct
Capital Costs
Resource
CaptialCost ($US1999/kW) Geothermal
$1,150–$3,000
Hydropower
$735–$4,778 Coal
$1,070–$1,410
Nuclear
$1,500–$4,000
Operating and Maintenance Cost
Table 5. Geothermal Operating and Maintenance Costs
by Plants Size (U.S. cents/kWh)30
(<5 MW)
(>30 MW)
As shown by Table 6, geothermal operating costs of 0.4–1.4 ¢/kWh are within
the range of O&M costs of conventional power plants.
Table 6. Opeating and Maintenance Cost
Comparison
by Baseload Power Source (U.S. cents/kWh)
The levelized cost of power production is the
average cost of power production over the life of a power plant, taking into
account all capital expenses and operating and maintenance costs, as well as
fuel costs for power plants that rely on external fuel sources. Major factors
affecting geothermal power cost are the depth and temperature of the
resource, well productivity, environmental compliance, project infrastructure
and economic factors such as the scale of development, and project financing
costs.
of Baseload Power by Source
(U.S. cents/kWh)
In 1996, the U.S. geothermal energy industry as a whole provided
approximately 12,300 direct jobs in the United States, and an additional
27,700 indirect jobs in the United States. The electric generation part of
the industry employed about 10,000 people to install and operate geothermal
power plants in the United States and abroad, including power plant
construction and related activities such as exploration and drilling;
indirect employment was about 20,000.37 Table 8 provides estimates
of job creation from renewable energy development based on existing and
planned projects in California and the market outlook of project developers
and equipment manufacturers. Natural gas is included in the table because the
bulk of new nonrenewable generation is expected to rely upon natural gas. The
table indicates that geothermal and landfill methane energy generation yields
significantly more jobs per MW of installed capacity than do natural gas
plants.
Table 8. Employment Rates by Energy Technology38,39
Economic Impacts
One of the most important economic aspects of geothermal energy is that it is
generated with indigenous resources, reducing a nation’s dependence on
imported energy, thereby reducing trade deficits. Reducing 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 displaced with
domestic energy resources.
Nearly half of the developing countries have rich geothermal resources, which
could prove to be an important source of power and revenue.42
Geothermal projects can reduce the economic pressure of developing country
fuel imports and can offer local infrastructure development and employment.
For example, the Philippines have exploited local geothermal resources to
reduce dependence on imported oil, with installed geothermal capacity and
power generation second in the world after the United States. In the late
1970s, the Philippine government instituted a comprehensive energy plan,
under which hydropower, geothermal energy, coal, and other indigenous
resources were developed and substituted for fuel oil, reducing their
petroleum dependence from 95% in the early 1970s to 50% by the mid-1980s.43

Source:
U.S.
Department of Energy, http://www.eia.doe.gov/kids/renewable/geothermal.html.
Because the geologic processes known as
plate
tectonics, the Earth’s crust has been broken into 12 huge plates
that move apart or push together at a rate of millimeters per year. Where two
plates collide, one plate can thrust below the other, producing extraordinary
phenomena such as ocean trenches or strong earthquakes. At great depth, just
above the down going plate, temperatures become high enough to melt rock,
forming magma.3 Because magma is less dense than surrounding
rocks, it moves up toward the earth’s crust and carries heat from below.
Sometimes magma rises to the surface through thin or fractured crust as lava.Resource Identification
Once potential geothermal resources have been identified, exploratory
drilling is carried out to further quantify the resource. Because of the high
temperature and corrosive nature of geothermal fluids, as well as the hard
and abrasive nature of reservoir rocks found in geothermal environments,
geothermal drilling is much more difficult and expensive than conventional
petroleum drilling. Each geothermal well costs $1–4 million to drill, and a
geothermal field may consist of 10–100 wells. Drilling can account for 30–50%
of a geothermal project’s total cost.7 Typically,
geothermal wells are drilled to depths ranging from 200 to 1,500 meters depth
for low- and medium-temperature systems, and from 700 to 3,000 meters depth
for high-temperature systems. Wells can be drilled vertically or at an angle.
Wells are drilled in a series of stages, with each stage being of smaller
diameter than the previous stage, and each being secured by steel casings,
which are cemented in place before drilling the subsequent stage. The final
production sections of the well use an uncemented
perforated liner, allowing the geothermal fluid to pass into the pipe. The
objectives of this phase are to prove the existence of an exploitable resource
and to delineate the extent and the characteristics of the resource. An
exploratory drilling program may include shallow temperature-gradient wells,
“slim-hole” exploration wells, and production-sized exploration/production
wells. Temperature-gradient wells are often drilled from 2–200 meters in
depth with diameters of 50–150 mm. Slim-hole exploration wells are usually
drilled from 200 to 3000 meters in depth with bottom-hole diameters of 100 to
220 mm. The size and objective of the development will determine the number
and type of wells to be included in exploratory drilling programs.8
http://www.eere.energy.gov/geothermal
National Renewable Energy Laboratory: Geothermal Technologies Program
http://www.nrel.gov/geothermal/geoelectricity.html
International
Programs
Philippines Department of Energy
http://www.doe.gov.ph
The World Bank Group
http://www.worldbank.org/html/fpd/energy/geothermal
Industry Associations
Geothermal Energy Association
http://www.geo-energy.org
Geothermal Resources Council
http://www.geothermal.org
International Geothermal Association
http://iga.igg.cnr.it
Nonprofit
Organizations
Marin County Geothermal Education Office
http://www.geothermal.marin.org
Renewable Northwest Project
http://www.rnp.org/RenewTech/tech_geo.html
Technical
Information
University of Utah Energy & Geoscience
Institute
http://egi-geothermal.org
Idaho National Engineering and Environmental Laboratory
http://geothermal.id.doe.gov
Oregon Institute of Technology
http://geoheat.oit.edu
Geothermal
Resource Assessment
Geothermal Energy Research State Maps
http://geothermal.id.doe.gov/maps-software.shtml
United States Geothermal Potential http://www.eere.energy.gov/geopoweringthewest/geomap.html
Opportunities for Near-Term Geothermal Development on Public Lands in the
Western United States (CD-ROM)
http://www.nrel.gov/docs/fy03osti/33105.pdf
U.S. Geothermal Projects and Resource Areas
http://geoheat.oit.edu/dusys.htm
Additional
Resources
http://www.geo-energy.org/Links.htm
http://iga.igg.cnr.it/links.php

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