Buoyancy-driven flow in a confined aquifer with a vertical gradient of permeability
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Publication:4582937
DOI10.1017/JFM.2018.375zbMath1404.76258OpenAlexW2805050338WikidataQ129723300 ScholiaQ129723300MaRDI QIDQ4582937
Edward M. Hinton, Andrew W. Woods
Publication date: 27 August 2018
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://www.repository.cam.ac.uk/handle/1810/279560
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Cites Work
- Unnamed Item
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- New high-resolution central schemes for nonlinear conservation laws and convection-diffusion equations
- Post-injection spreading and trapping of CO\(_{2}\) in saline aquifers: Impact of the plume shape at the end of injection
- On the slow draining of a gravity current moving through a layered permeable medium
- Two-phase gravity currents in porous media
- On the flow of buoyant fluid injected into a confined, inclined aquifer
- Gravity currents in horizontal porous layers: transition from early to late self-similarity
- Buoyancy-dominated displacement flows in near-horizontal channels: the viscous limit
- Capillary entry pressure and the leakage of gravity currents through a sloping layered permeable rock
- Gravity-driven flows in porous layers
- Miscible displacement in a Hele-Shaw cell at high rates
- The competition between gravity and flow focusing in two-layered porous media
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