A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equations at large values of the Rayleigh number Ra is performed to gain insight into two-dimensional porous medium convection in domains of varying aspect-ratio L. The steady convective states are shown to transport less heat than the statistically steady ‘turbulent’ flow realised at the same parameter values: the Nusselt number Nu∼Ra for turbulent porous medium convection, while Nu∼Ra 0.6 for the maximum heat-transporting steady solutions. A key finding is that the lateral scale of the heat-flux-maximising solutions shrinks roughly as L∼Ra−0.5, reminiscent of the decrease of the mean inter-plume spacing observed in turbulent porous medium convec...
Numerical simulations are used to probe Rayleigh-Darcy convection in fluid-saturated porous media t...
Here we investigate the effect of the vertical rate of change in thermal diffusivity due to a hydrot...
The Darcy–Boussinesq equations at infinite Darcy–Prandtl number are used to study convection and hea...
A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equat...
A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equat...
A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equat...
Convection in a porous medium at high Rayleigh number Ra exhibits a striking quasisteady columnar st...
Buoyancy-driven convection in fluid-saturated porous media is a key environmental and technological ...
This paper outlines a combined theoretical and numerical study of the mass transfer effected by high...
We perform large-scale numerical simulations to study Rayleigh-Darcy convection in three-dimensional...
Porous geological formations are commonly interspersed with thin, roughly horizontal, low-permeabili...
Convection in a closed domain driven by a dense buoyancy source along the upper boundary soon starts...
Convection in a closed domain driven by a dense buoyancy source along the upper boundary soon starts...
We present a numerical study of convection in a horizontal layer comprising a fluid-saturated porous...
Numerical simulations are used to probe Rayleigh-Darcy convection in fluid-saturated porous media to...
Numerical simulations are used to probe Rayleigh-Darcy convection in fluid-saturated porous media t...
Here we investigate the effect of the vertical rate of change in thermal diffusivity due to a hydrot...
The Darcy–Boussinesq equations at infinite Darcy–Prandtl number are used to study convection and hea...
A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equat...
A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equat...
A systematic investigation of unstable steady-state solutions of the Darcy–Oberbeck–Boussinesq equat...
Convection in a porous medium at high Rayleigh number Ra exhibits a striking quasisteady columnar st...
Buoyancy-driven convection in fluid-saturated porous media is a key environmental and technological ...
This paper outlines a combined theoretical and numerical study of the mass transfer effected by high...
We perform large-scale numerical simulations to study Rayleigh-Darcy convection in three-dimensional...
Porous geological formations are commonly interspersed with thin, roughly horizontal, low-permeabili...
Convection in a closed domain driven by a dense buoyancy source along the upper boundary soon starts...
Convection in a closed domain driven by a dense buoyancy source along the upper boundary soon starts...
We present a numerical study of convection in a horizontal layer comprising a fluid-saturated porous...
Numerical simulations are used to probe Rayleigh-Darcy convection in fluid-saturated porous media to...
Numerical simulations are used to probe Rayleigh-Darcy convection in fluid-saturated porous media t...
Here we investigate the effect of the vertical rate of change in thermal diffusivity due to a hydrot...
The Darcy–Boussinesq equations at infinite Darcy–Prandtl number are used to study convection and hea...