For the constant-entrainment axisymmetric plume equations , with , pure balance means at every height. This is a similarity relation between fluxes, not a requirement that the physical source have zero radius. A finite source on this curve is represented by a plume virtual origin. For fluxes normalized by pi and top-hat fields, the same relation is .
When and are constant, eliminating height between and gives . Thus is constant. Its sign classifies forced and lazy departures from pure plume balance, and its vanishing makes a finite-source plume exactly self-similar after a virtual-origin shift.
For an axisymmetric top-hat plume model in uniform ambient density, use full kinematic fluxes and . The equations , conserve . Solve this invariant for , then integrate to obtain the displayed exact quadrature. It determines the transition from the near-source jet limit of the top-hat plume model to the distant pure plume. The two regimes cannot be added by linear superposition because the flux equations are nonlinear.
For positive source fluxes and positive constant buoyancy flux, the plume flux-balance invariant has a finite constant while grows without bound. Dividing by makes the source imbalance vanish relatively. The balances then give and . This attraction concerns relative similarity and does not assert that different finite sources share the same virtual origin.
The dimensionless ratio compares a plume to the constant-entrainment pure balance. Values one, below one and above one describe pure plume balance, a momentum-excess forced plume, and a momentum-deficient lazy plume, respectively. For fluxes normalized by pi and a top-hat profile, .
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