The Batchelor entrainment hypothesis takes the inflow speed through the plume's exposed outer edge to be , where is the entrainment coefficient. A wall plume has only one such edge, so .
The Boussinesq approximation replaces density by a constant reference value in inertia and mass flux while retaining the small density deficit in buoyancy. It requires . A sufficiently hot radiator can violate this near the source, where thermal expansion is large and the developed-plume description may also fail.
Put for the kinematic buoyancy flux per unit length. Dimensional analysis for a line plume gives
The plume rise time is therefore . Changing the room stratification requires a plume volume comparable with , so . Hence
The plume consequently follows the slowly changing ambient through a quasi-steady approximation when .
The Boussinesq approximation replaces density by a common reference value in inertia, mass conservation, and pressure acceleration, while retaining small density differences in the gravitational buoyancy term. It gives incompressible flow and is appropriate here when
even though those small differences drive the room-scale motion. It would fail for order-one thermal density contrasts or strongly compressible ventilation.
The Batchelor entrainment hypothesis sets the mean inflow speed across a turbulent plume edge to times a representative axial plume speed, where is the entrainment coefficient. It closes integral plume balances by relating plume growth to its speed. Applied here, it produces an entraining axisymmetric warm plume above the floor source and a one-sided cold wall line plume below the vent. Treating both as turbulent top-hat plume models neglects source regions, detailed profiles, wall friction, interaction between the two plumes, and the finite thickness of the density interface; these are the principal modelling assumptions.