Bachelorarbeit, 2004
74 Seiten, Note: 2.0 (B)
1. Introduction
1.1. Use of natural heat of the earth until today
1.2. Definition of geothermal energy
2. Main features of geothermal energy
2.1. The different types of geothermal energy sources
2.2. Technology of geothermal energy and technological problems in connection with possible ecological effects
2.2.1. Hydrothermal energy technology
2.2.2. Hot dry rock method
2.2.3. Shallow geothermal application systems
2.3. Legal and political aspects
2.3.1. Legal requirements
2.3.2. Energy political measures
3. Geothermal energy in Brandenburg
3.1. Geology of Brandenburg
3.1.1. Character of the landscape
3.1.2. Present day climatic condition
3.1.3. Geological and hydrological overview of Brandenburg
3.1.4. Relations between tectonic structure and temperature distribution in Brandenburg
3.1.5. The temperature distribution in Brandenburg
3.1.6. Chemical composition of thermal water in Brandenburg
3.2. Geothermal potential of Brandenburg
3.3. Application of geothermal energy in Brandenburg now and then
3.4. Economical aspects
3.5. Current projects in Brandenburg
3.6. Possible future development
4. Conclusion
The primary objective of this bachelor thesis is to evaluate the technical, geological, and economic potential of geothermal energy in the state of Brandenburg, Germany. The research addresses the current status of geothermal utilization, the technological requirements for various applications, and the legal and political framework necessary to promote geothermal energy as a viable renewable energy source in the region.
1.1. Usage of natural heat of the earth until today
The heat in the inner of the earth has always been a matter of consideration in human life. The oldest kind to utilise geothermal energy is the use of warm water in baths. A first peak in using geothermal heat was during the Roman Empire in Europe and in the eastern Mediterranean region in form of thermal baths. In regions of cold and temperate climate like Iceland having geological favourable sites, other possibilities for the use of geothermal energy were found out like cooking and heating. Although the importance of spas and thermal baths is still increasing today, the significance of geothermal energy as substitute for fossil energy sources is much higher nowadays. Since the dependence on limited fossil energy sources was understood the relevance of renewable energies as primary energy carrier has been increasing rapidly (Buntebarth, 1980).
During the 18th century the first investigation and calculations were taking place with regard to the temperature distribution below the surface. Starting with hypothetical assumptions about the heat inside the earth by many scientists like Descartes, Leibniz and later Fourier the research of geothermal heat began which is today a part of geophysics. The first practical application of geothermal energy was carried out in 1827 in Laderello, Italy heating a tank for the production of boric acid. In Laderello the generation of electric power out of geothermal energy began in 1904 (Kühn, 1988). In 1912 the first generator with an installed capacity of 250 kW was used economically fed by hot vapour. Today two power units with each 150 MW installed capacity are in operation, using a hydrothermal steam reservoir in 3000 meters depth.
1. Introduction: Provides an overview of the historical use of geothermal energy and defines the basic scientific concept of geothermal heat.
2. Main features of geothermal energy: Discusses different geothermal energy sources, technical methods for heat extraction, and the legal and political framework in Germany.
3. Geothermal energy in Brandenburg: Analyzes the specific geology, temperature distribution, economic aspects, and current pilot projects regarding geothermal use in Brandenburg.
4. Conclusion: Summarizes the potential for future geothermal energy use in the region and assesses the role of economic factors versus current technological capabilities.
Geothermal Energy, Brandenburg, Renewable Energy, Hydrothermal Systems, Hot Dry Rock, Heat Pumps, Geological Potential, Energy Policy, Thermal Water, Sustainable Energy, Deep Drilling, Tectonic Structure, Economic Feasibility.
The thesis focuses on evaluating the geothermal potential of the state of Brandenburg, covering geological, technological, and economic perspectives for both shallow and deep geothermal energy.
The work distinguishes between shallow geothermal systems, hydrothermal low- and high-enthalpy systems, and the hot dry rock method.
The goal is to determine if geothermal energy can act as a viable substitute for fossil fuel-based energy in Brandenburg by analyzing existing technology and political support mechanisms.
The study utilizes a review of existing technical literature, an analysis of geological data (temperature gradients, reservoir characteristics), and an economic evaluation of current heat plant projects.
The main part covers the geological stratification of Brandenburg, the temperature distribution in the subsurface, current operational projects (e.g., in Prenzlau and Groß Schönebeck), and economic cost analyses.
Key terms include geothermal energy, Brandenburg, geological potential, heat pumps, renewable energy, and hydrothermal reservoirs.
The chimney effect refers to the phenomenon where specific geological structures, such as salt stocks, influence local temperature fields due to their high thermal conductivity compared to surrounding rocks.
The author notes that while hot dry rock has high potential, its economic viability is currently constrained by high exploration costs and the need for further technological development in rock stimulation.
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