The near-field shape and stability of a porous plume

TL;DR

This paper investigates the near-field shape and stability of porous plumes formed by fluid injection, revealing how injection rate influences steady state formation and stability, with implications for CO2 sequestration.

Contribution

It demonstrates that near-field plume shape depends on a single dimensionless parameter and provides a linear stability analysis of the plume under different velocity ratios.

Findings

Steady plume forms at moderate injection rates matching buoyancy velocity.

Instability and breakup occur at very small injection rates due to density contrast.

Plume stability depends on the ratio of inlet to buoyancy velocity.

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 only depends 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.