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 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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