Homuth, S. ; Rühaak, W. ; Bär, K. ; Sass, I. (2013)
Medium Deep High Temperature Heat Storage.
In: Proceedings of the European Geothermal Congress, Pisa, Italy
Buchkapitel, Bibliographie
Kurzbeschreibung (Abstract)
Heating of buildings requires more than 25 % of the total end energy consumption in Germany. Shallow geothermal systems for indirect use as well as shallow geothermal heat storage systems like aquifer thermal energy storage (ATES) or borehole thermal energy storage (BTES) typically provide low exergy heat. The temperature levels and ranges typically require a coupling with heat pumps. By storing hot water from solar panels or thermal power stations with temperatures of up to 110 °C a medium deep high temperature heat storage (MDHTS) can be operated on high temperature levels which are characterized by 50 °C to 110 °C. Therefore, heat pumps are not necessary and low temperature space heating systems are not mandatory because MDHTS can be operated in conjunction with classical radiator based high temperature heating systems. Furthermore, storage depths of 500 m to 1,500 m below surface avoid conflicts with groundwater use for drinking water or other purposes. Additionally, the temperature difference between the storage system and the surrounding rocks becomes smaller with increasing depth resulting in a decrease of thermal losses. Permeability is typically also decreasing with greater depth, especially in the crystalline basement therefore conduction becomes the dominant heat transport process. Solar-thermal charging of a MDHTS is a very beneficial option for supplying heat in urban and rural systems. Feasibility and design criteria of different system configurations are discussed. One system is designed to store and supply heat (300 kW) for an office building. The required boreholes are located in granodioritic bedrock. Resulting from this setup several challenges have to be addressed. The drilling and completion has to be planned carefully under consideration of the geological and tectonical situation at the specific site. In addition to the MDHTS system the results of this drill site will help to characterize potential target horizons for petrothermal systems (Enhanced Geothermal Systems (EGS)) in the nearby Upper Rhine Graben where several deep geothermal projects are already in operation and new ones are planned which target the same geological formations like the one discussed here.
Typ des Eintrags: | Buchkapitel | ||||||||||||
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Erschienen: | 2013 | ||||||||||||
Autor(en): | Homuth, S. ; Rühaak, W. ; Bär, K. ; Sass, I. | ||||||||||||
Art des Eintrags: | Bibliographie | ||||||||||||
Titel: | Medium Deep High Temperature Heat Storage | ||||||||||||
Sprache: | Englisch | ||||||||||||
Publikationsjahr: | 2013 | ||||||||||||
Ort: | Pisa | ||||||||||||
Buchtitel: | Proceedings of the European Geothermal Congress, Pisa, Italy | ||||||||||||
URL / URN: | http://www.researchgate.net/publication/259019023_Medium_Dee... | ||||||||||||
Kurzbeschreibung (Abstract): | Heating of buildings requires more than 25 % of the total end energy consumption in Germany. Shallow geothermal systems for indirect use as well as shallow geothermal heat storage systems like aquifer thermal energy storage (ATES) or borehole thermal energy storage (BTES) typically provide low exergy heat. The temperature levels and ranges typically require a coupling with heat pumps. By storing hot water from solar panels or thermal power stations with temperatures of up to 110 °C a medium deep high temperature heat storage (MDHTS) can be operated on high temperature levels which are characterized by 50 °C to 110 °C. Therefore, heat pumps are not necessary and low temperature space heating systems are not mandatory because MDHTS can be operated in conjunction with classical radiator based high temperature heating systems. Furthermore, storage depths of 500 m to 1,500 m below surface avoid conflicts with groundwater use for drinking water or other purposes. Additionally, the temperature difference between the storage system and the surrounding rocks becomes smaller with increasing depth resulting in a decrease of thermal losses. Permeability is typically also decreasing with greater depth, especially in the crystalline basement therefore conduction becomes the dominant heat transport process. Solar-thermal charging of a MDHTS is a very beneficial option for supplying heat in urban and rural systems. Feasibility and design criteria of different system configurations are discussed. One system is designed to store and supply heat (300 kW) for an office building. The required boreholes are located in granodioritic bedrock. Resulting from this setup several challenges have to be addressed. The drilling and completion has to be planned carefully under consideration of the geological and tectonical situation at the specific site. In addition to the MDHTS system the results of this drill site will help to characterize potential target horizons for petrothermal systems (Enhanced Geothermal Systems (EGS)) in the nearby Upper Rhine Graben where several deep geothermal projects are already in operation and new ones are planned which target the same geological formations like the one discussed here. |
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Zusätzliche Informationen: | Pisa, Italy, 3‐7 June 2013 |
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Fachbereich(e)/-gebiet(e): | 11 Fachbereich Material- und Geowissenschaften 11 Fachbereich Material- und Geowissenschaften > Geowissenschaften 11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Angewandte Geothermie |
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Hinterlegungsdatum: | 16 Nov 2015 08:59 | ||||||||||||
Letzte Änderung: | 28 Mai 2024 11:24 | ||||||||||||
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