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- W2907557104 abstract "The chapter deals with changing rates of gas migration to the earth's surface, which may signal the development of ground subsidence. Subsidence often occurs due to man's need for fresh water; and oil and gas to satisfy domestic, industrial, and agricultural demands. Withdrawal of the fluids from a petroleum reservoir or an aquifer reduces the pore pressure and results in the increase in effective stress. Thus, compaction of reservoir rocks occurs and to balance the existing overburden pressure, the overlying formations and the land surface subside. The primary cause of subsidence is rock compaction. Compaction is the result of several simultaneously acting phenomena that are induced by the increase of effective stress in the rocks in which the pore-pressure is reduced due to fluid withdrawal. Presence of shale and clay beds within the productive zone can significantly contribute to the overall reservoir compaction. Compaction takes place over a long period of time because the process involves the slow expulsion of water. Shallow reservoirs will undergo viscous creep, deforming horizontally as well as vertically if the overburden pressure is principally supported by the grain-to-grain stress over a long period of time. Subsiding bowl develops slowly, over a very large area with structures inclining toward the center of the subsiding bowl and fractures developing at the periphery." @default.
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- W2907557104 date "2000-01-01" @default.
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- W2907557104 title "Interrelationships among Subsidence, Gas Migration, and Seismic Activity" @default.
- W2907557104 doi "https://doi.org/10.1016/b978-088415430-3/50022-7" @default.
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