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- W45642764 abstract "On the basis of the two-dimensional theory of elasticity, the opening of a fault and the resulting slip due to injection of fluid are studied for the extraction of geothermal heat from hot dry rock masses. A fault is modeled by a plane of frictional contact between two elastic bodies. Once fluid is injected between the two surfaces of a fault plane, it will be opened up over a region where the pressure acting on the fault plane before the injection is locally smaller than that of neighboring regions. The size of the opened region, i.e., the fluid-filled region, is compared with that of a vertical, fluid-filled crack within the earth’s crust to show that the fluid-filled region could be used as a reservoir for the extraction of geothermal heat. As the opening takes place, slip spreads simultaneously along the fault plane due to the reduction of frictional forces in the fluid-filled region. This slip is analyzed by the use of two models for the fault plane, i.e., an interface with frictional resistance only, and an interface with both frictional resistance and fracture toughness for the sliding mode. It is shown that the two models do not exhibit any significant difference in the size of the slipped region when the fluid-filled region is of dimensions of practical interest." @default.
- W45642764 created "2016-06-24" @default.
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- W45642764 date "1983-01-01" @default.
- W45642764 modified "2023-09-28" @default.
- W45642764 title "A Reservoir Created by Injection of Fluid on a Fault for the Extraction of Geothermal Heat" @default.
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- W45642764 doi "https://doi.org/10.1007/978-94-009-6884-4_30" @default.
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