The near-field shape and stability of a porous plume

Abstract

When a fluid is injected into a porous medium saturated with an ambient fluid of a greater density, the injected fluid forms a plume that rises upwards due to buoyancy. In the near field of the injection point, the plume adjusts its speed to match the buoyancy velocity of the porous medium, either thinning or thickening to conserve mass. These adjustments are the dominant controls on the near-field plume shape, rather than mixing with the ambient fluid, which occurs over larger vertical distances. In this study, we focus on the plume behaviour in the near field, demonstrating that for moderate injection rates, the plume will reach a steady state, whereby it matches the buoyancy velocity over a few plume width scales from the injection point. However, for very small injection rates, an instability occurs in which the steady plume breaks apart due to the insurmountable density contrast with the surrounding fluid. The steady shape of the plume in the near field depends only on a single dimensionless parameter, which is the ratio between the inlet velocity and the buoyancy velocity. A linear stability analysis is performed, indicating that for small velocity ratios, an infinitesimal perturbation can be constructed that becomes unstable, whilst for moderate velocity ratios, the shape is shown to be stable. Finally, we comment on the application of such flows to the context of CO $_2$ sequestration in porous geological reservoirs.

Anisotropy distorts the spreading of a fixed volume porous gravity current

“…The former condition matches the pressure in the fluid with the ambient hydrostatic pressure (note that the reference pressure p a is the ambient value at z = 0), while the latter condition imposes that a particle at the interface remains at the interface [24,25].…”

Study on the fountain effect of the bubble plume formed by submarine gas pipeline leakage

“…The physical characteristics of the fountain are related to the release and diffusion of the bubble plume in the water (Cardoso and Cartwright, 2024). To analyze the physical characteristics of the fountain formed by the bubble plume on the water surface, the researchers mainly use integral model and computational fluid dynamics (Johansen, 2000;Benham, 2023;Garvey and Fowler, 2024). The integral model describes the radial velocity distribution of the plume in accordance with the Gaussian distribution, indicating that the fountain shape is inverted conical (Nazir et al, 2008 andAfenyo et al, 2017).…”