DNS of Rayleigh-Darcy convection up to Ra=10^6 shows linear Nu-Ra scaling with a slope change at Ra≈4×10^5 marking the ultimate regime, accompanied by protoplume-to-megaplume evolution and boundary-layer thinning.
Miscible rectilinear displacements with gravity override
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Ultimate regime in Rayleigh-Darcy Convection
DNS of Rayleigh-Darcy convection up to Ra=10^6 shows linear Nu-Ra scaling with a slope change at Ra≈4×10^5 marking the ultimate regime, accompanied by protoplume-to-megaplume evolution and boundary-layer thinning.