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- W1969217013 abstract "We examine the motion of a buoyant fluid injected into a water-saturated porous rock as it spreads along a thin inclined low-permeability barrier. We account for leakage of the fluid across the barrier once the current is sufficiently deep so that the pressure exceeds the capillary threshold. We show that at some distance from the source, the pressure decreases below this threshold, and all the remaining flux spreads laterally along the barrier. We examine the controls on the partitioning of the flow between the draining flux and the laterally spreading flux and also the controls on the lateral extent of the draining region for the case of an instantaneous release and a maintained release of fluid. We consider the implications of our work for the dispersal of CO 2 plumes which may be sequestered in deep saline aquifers." @default.
- W1969217013 created "2016-06-24" @default.
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- W1969217013 date "2009-01-10" @default.
- W1969217013 modified "2023-09-30" @default.
- W1969217013 title "Capillary entry pressure and the leakage of gravity currents through a sloping layered permeable rock" @default.
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- W1969217013 doi "https://doi.org/10.1017/s0022112008004527" @default.
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