A numerical study on the creation of artificial supercritical geothermal reservoirs by hydraulic fracturing

•Hydraulic fracturing at supercritical temperatures could create meaningful sized artificial reservoirs.•In-situ stress conditions and pre-existing weak faces have a significant impact on the progression of the stimulated zone.•The position of the artificial reservoir may be controlled by forming a...

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Veröffentlicht in:Geothermics 2022-11, Vol.105, p.102500, Article 102500
Hauptverfasser: Watanabe, Kimio, Watanabe, Norihiro, Watanabe, Noriaki, Sakaguchi, Kiyotoshi, Aichi, Masaatsu, Ouchi, Hisanao, Asanuma, Hiroshi
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Sprache:eng
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Zusammenfassung:•Hydraulic fracturing at supercritical temperatures could create meaningful sized artificial reservoirs.•In-situ stress conditions and pre-existing weak faces have a significant impact on the progression of the stimulated zone.•The position of the artificial reservoir may be controlled by forming a weak face before stimulation.•The injection of cold water may not prevent the creation of cloud-fracture networks.•The use of a short open-hole section in injection wells may be effective in reducing the time and amount of water. We developed a supercritical geothermal reservoir creation simulator that uses a simple 3D model. The simulator was based on an increase in permeability caused by hydraulic fracturing as confirmed in a laboratory experiment. The simulator does not simulate the fracture behavior in rocks; instead, the fracturing phenomenon is expressed as a rapid change in permeability. In this study, we evaluated rock mechanics such that changes in crustal stress associated with changes in pore pressure could be considered. Using the developed simulator, a simulation was performed for the creation of a reservoir using hydraulic fracturing. The results showed that a target artificial reservoir with a radius of hundreds of meters could be formed through hydraulic fracturing. Furthermore, the state of the initial crust stress had a major impact on reservoir creation.
ISSN:0375-6505
1879-3576
DOI:10.1016/j.geothermics.2022.102500