Buoyancy Effects on Upward Brine Displacement Caused by CO2 Injection

Upward displacement of brine from deep reservoirs driven by pressure increases resulting from CO 2 injection for geologic carbon sequestration may occur through improperly sealed abandoned wells, through permeable faults, or through permeable channels between pinch-outs of shale formations. The conc...

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Veröffentlicht in:	Transport in porous media 2011-03, Vol.87 (2), p.525-540
Hauptverfasser:	Oldenburg, Curtis M., Rinaldi, Antonio Pio
Format:	Artikel
Sprache:	eng
Schlagworte:	ABANDONED WELLS AQUIFERS BRINES Carbon dioxide CARBON SEQUESTRATION Civil Engineering Classical and Continuum Physics Computer simulation Conduits Cooling Displacement Earth and Environmental Science Earth Sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Faults Geotechnical Engineering & Applied Earth Sciences GEOTHERMAL GRADIENTS Groundwater HEAT EXCHANGERS Hydrogeology Hydrology. Hydrogeology Hydrology/Water Resources HYDROSTATICS Industrial Chemistry/Chemical Engineering Intrusion Mathematical models Permeability Pollution, environment geology Reservoirs Saline water SALINITY Salt water SEDIMENTARY BASINS SHALES Steady state Two dimensional models WATER
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