Close physical analysis of free convection and the associated vertical buoyancy and density forces shows that they do not exist in a natural continental subsurface environment. All density and buoyancy derivedforces need to be included by modifying the length of the pressure potential forces of fresh...
free convectionlaminar boundary layercurvilinear coordinatesgreatest slope linegeneral integralgeodesic curvatureIn this paper, we derive a quasilinear second-order partial differential equation which has to be satisfied by surfaces around which 3D free convection boundary layer flows can be two-...