RENWABLE ENERGY INFORMATION HUB- Geothermal Energy

Oct 6, 07

Geothermal Energy – A Viable Source

Geothermal energy is energy derived from the heat of the earth’s core. It is clean, abundant, and reliable. If properly developed, it can offer a renewable and sustainable energy source. There are three primary applications of geothermal energy: electricity generation, direct use of heat, and ground-source heat pumps. Direct use includes applications such as heating buildings or greenhouses and drying foods, whereas ground source heat pumps are used to heat and cool buildings using surface soils as a heat reservoir. This paper covers the use of geothermal resources for production of utility-scale electricity and provides an overview of the history, technologies, economics, environmental impacts, and policies related to geothermal power.

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
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

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.


Table 5. Geothermal Operating and Maintenance Costs
by Plants Size (U.S. cents/kWh)
30

Cost Component

Small Plants
(<5 MW)

Medium Plants (5–30 MW)

Large Plants
(>30 MW)

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


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)

Resource

O&M Cost (cents/kWh)

Geothermal

0.4–1.4

Hydropower31

0.7

Coal32

0.46

Nuclear33

1.9

Levelized Cost
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.

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
of
Baseload Power by Source

Resource

Levelized Cost36
(U.S. cents/kWh)

Geothermal

1.5–7.0

Hydropower

0.5–2.4

Coal

2.0–5.0

Nuclear

1.5–3.0

Job Creation

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

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


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.

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
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

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.
Source:
U.S. Department of Energy, http://www.eia.doe.gov/kids/renewable/geothermal.html.

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

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.

 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.

Resource Identification

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

  1. Identification of geothermal phenomena
  2. Ascertaining that a useful geothermal production field exists
  3. Estimation of the size of the resource
  4. Classification of the geothermal field
  5. Location of productive zones
  6. Determination of the heat content of the fluids that will be discharged by the wells in the geothermal field
  7. Compilation of a body of data against which the results of future monitoring can be viewed
  8. Assessment of the pre-exploitation values of environmentally sensitive parameters
  9. Determination of any characteristics that might cause problems during field development

Drilling
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

Sources of Further Information

U.S. Government Programs

U.S. Department of Energy
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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