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Geothermal energy info
Geothermal energy info
Important sources of geothermal energy
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Geothermal energy is the harvesting of heat energy stored in the inner depth of the Earth’s crust [1]. This internal heat comes from two primary sources: radioactive decay of elements and primordial heat resulting from the initial formation of the Earth [2]. The earth’s outer layer acts as an insulator to the heat, which is why geothermal energy involves digging deep into the soil and pumping the heat from those hotter zones.
Heat resources are not evenly distributed under the Earth’s surface. The highest quality superficial geothermal resources are mainly located in regions with high tectonic activity, such as the Pacific ‘Ring of Fire’ [2]. For this reason, the highest potential for natural geothermal sourcing in Canada lies in the western provinces, especially in the provinces of British Columbia and Yukon [3].
Those zones have the highest heat concentration and can be used for the generation of electrical power.
In lower temperature regions, heat energy can be pumped for direct-use in heating applications, such as thermal hot springs, or heating of commercial and residential buildings. This last process is termed geo-exchange.
With current technologies, electricity production from geothermal sources requires temperatures of 100˚C or higher, as well as an existing underground hydrothermal reservoir [3]. Flash steam power plants, which operate in hot spots with the highest temperatures simply draw the hot water from the soil and use it to drive a regular power generating steam turbine. In lower temperature locations, a Binary Cycle Power Plant is used, in which the hot water heats a binary liquid with a lower boiling temperature [2].
Availability Technology Output
10°C Everywhere Heat pump Heating homes, spa
50°C Everywh...
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...thermal energy. Energies, 3(8), 1443-1471.
5. Holroyd, P. (2011). Geothermal Energy: A No-Brainer for Canada. Pembina Institute. Retrieved from: http://www.pembina.org/
6. Thompson, A. (2010). Geothermal Development in Canada: country update. In Proceedings World Geothermal Congress, Bali, Indonesia.
7. Holroyd, P., Dagg, J., & Franchuk, R. (2011). Building a regulatory framework for geothermal energy development in the NWT. Pembina Institute for Appropriate Development.
8. Ghomshei, M. M., & Eng, P. (2007). Geothermal energy from Con Mine for heating the city of Yellowknife, NWT: A concept study. Retrieved from: http://www.yellowknife.ca/
9. Ferguson, G., & Grasby, S. E. (2014). The geothermal potential of the basal clastics of Saskatchewan, Canada. Hydrogeology Journal, 22(1), 143-150.
10. C. I. A. (2010). The world factbook. Retrieved from: http://www.cia.gov/
The Starved Rock Member of the Saint Peter Sandstone is preserved as a northeast-southwest trending belt of strata that is ...
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
"Geology Fieldnotes - Katmai National Park and Preserve." National Park Service: Nature & Science» Geology Resources Division. 01 Apr. 2005. Web. Feb. 2014.
Ŝibrava, V., Bowmen, D.Q., and Richmond, G.M, 1986, Quaternary glaciations in the northern hemisphere; report of the International Geological Correlation Programme, Project 24 (International Union of Geological Sciences and UNESCO): Pergamon Press, Oxford, New York, 514 p.
Chapter 2: Canada’s Physical Base emphasizes reasoning for which its physical geography attributes to its regional geography, along with the population distribution and developing core regions. This chapter outlines main geological structure, landforms, climate, and impact on human a...
The author discusses the enticement to political groups because of geoengineering’s alleged potential to reverse global warming rapidly and cheaply, as he presents concern regarding the significant risks and the threat of technology gone wrong. The author looks at the basic authority issues raised by geoengineering, its possible functions, governance, and specifically addresses inadequate research funding, rejection, and unilateral vs individual action. Bodansky is a professor at Arizona State University Sandra Day O 'Connor College of Law and has written three books and dozens of articles and book chapters on international law, international environmental law and climate change policy. This article will be a useful tool in discovering
Wood and Kienle, 1990, Volcanoes of North America: United States and Canada: Cambridge University Press, 354 p., p. 158-160, Contribution by Patrick Pringle.
Smith, C. (2009). How things work: Canada's oil sands. United Nations University, Vol.1, No. 110. Retrieved on December, 24, 2013 from
Mining in the Canadian Shield is an issue which should not be taken lightly. Many Canadians are concerned as to how the minerals are mined
...Kroeker designed the first commercial geothermal heat pump to heat the Commonwealth Building in Portland, Oregon and demonstrated it in 1946. 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. The original turbine lasted for more than 30 years and produced 11 MW net power. The binary cycle power plant was first demonstrated in 1967 in the U.S.S.R. and later introduced to the U.S. in 1981. This technology allows the generation of electricity from much lower temperature resources than previously. (Wikipedia, 2011)
However, nuclear energy is not the only source of energy that can produce a plethora of energy. There are not only cheaper options, but safer ones as well. Nuclear disaster are devastating events and will have massive implications on the environment. Also, the long term storage of nuclear waste is a problem that still exists and has not been solved for sixty years. Hydroelectric energy is not only che...
Inside Earth there is heat from pressure (push your hands together very hard). and feel the heat). There is heat from friction (rub your hands). together and feel the heat). There is also heat from radioactive decay.
For the generation of electricity, hot water, at temperatures ranging from about 700 degrees F, is brought from the underground reservoir to the surface through production wells, and is flashed to steam in special vessels by release of pressure. The steam is separated from the liquid and fed to a turbine engine, which turns a generator. In turn, the generator produces electricity. Spent geothermal fluid is injected back into peripheral parts of the reservoir to help maintain reservoir pressure. If the reservoir is to be used for direct-heat application, the geothermal water is usually fed to a heat exchanger before being injected back into the earth. Heated domestic water from the output side of the heat exchanger is used for home heating, greenhouse heating, vegetable drying and a wide variety of other uses.
Saini, Keshav. "Solar Thermal Energy Pros and Cons | Environmental Issues." Environmental Issues Blog. N.p., 6 Jan. 2012. Web. 04 Mar. 2014. .
inferred for the reservoir (4). The magma ascent to the surface occurred through a conduit of possibly 70 to 100 m in diameter (5). A thermal model predicts that such a reservoir should contain a core of partially molten magma (6) that can be detected by high-resolution seismic tomography.