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- W2541307387 abstract "Geothermal reservoirs are studied in their undisturbed natural state. First the hydrostatic state is investigated, which is valid invariably for both porous and fractured reservoirs. The compaction of a porous sedimentary reservoir induces the natural movement of the pore fluid. Because of the flow resistance, a slight overpressure is developed. Impermeable cap rock can prevent the vertical fluid movement, thus large overpressure arises in the reservoir." @default.
- W2541307387 created "2016-11-04" @default.
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- W2541307387 date "2017-01-01" @default.
- W2541307387 modified "2023-10-13" @default.
- W2541307387 title "Natural State of Undisturbed Geothermal Reservoirs" @default.
- W2541307387 doi "https://doi.org/10.1016/b978-0-12-800277-3.00005-0" @default.
- W2541307387 hasPublicationYear "2017" @default.
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