Lazy plume 2026-10-06
A buoyant plume with insufficient momentum for the corresponding pure plume balance. In the constant-entrainment top-hat model it has plume balance parameter , unlike the momentum-excess forced plume. The equations accelerate the plume and drive the balance parameter toward one downstream. The definition depends on the chosen flux and entrainment convention; it is not merely a synonym for slow vertical speed.
If two equal pure plumes merge while keeping their common velocity and reduced gravity, conservation of cross-sectional area gives radius times the individual radius. All three integral fluxes double. The plume balance parameter increases by , so the immediate combined plume is a lazy plume. Similarity attraction may restore pure balance farther downstream, but instantaneous pure balance does not follow from adding two pure plumes.
Use and constant entrainment parameter . The printed integrals are normalized by , so a top-hat plume model has , and ; the physical area is still . Keeping this normalization avoids spurious factors of in the flux equations.
Eliminate height between the two flux balances. The plume flux-balance invariant follows from
so
For positive fluxes, both and increase. In particular , so as . Therefore , whatever the finite source imbalance, and . Integrating gives the attracting similarity solution
This proves attraction to pure plume similarity for physical positive source fluxes. Sources with a vanishing initial volume or momentum flux enter the positive regime immediately and can be obtained by the corresponding limiting solutions; a point buoyancy source has the same similarity form with zero virtual-origin offset. The statement assumes positive buoyancy flux: a jet with is a different asymptotic problem.
Define the plume balance parameter
Pure plume balance means at each height, or equivalently : momentum, buoyancy and entrainment have their similarity relation, even when the source has finite radius. A forced plume has , meaning excess momentum relative to this balance; a lazy plume has , meaning insufficient momentum. The invariant ensures that the sign of the imbalance is preserved while . In particular, a strictly positive source remains pure at every height precisely when
For this source the exact solution is the same similarity form with replaced by . Writing ,
Thus the radius growth of an axisymmetric pure plume is and the plume virtual origin lies at , with . Equivalently, in terms of top-hat source properties, pure plume balance is .
For the stated source-to-source geometry, the relevant horizontal distance is . Consequently the edge criterion is , rather than the radius at which two expanding edges first touch. Since ,
Here . A positive merging height requires ; equality puts it at the source, while an already wider source satisfies the geometric condition from the start. The no-interaction premise extrapolates independent plumes even though their edges would first touch earlier, when each radius is .
Use with and to get . The individual plume properties at the specified height are therefore
The source volume flux affects the height through the virtual origin, but it does not affect these properties at a prescribed radius in an exactly pure plume.
For the stipulated merger of two equal pure plumes, the new radius is . This factor is outside , as required by the area. Since speed and reduced gravity are held fixed, the merged fluxes are , and . Their balance parameter is
The immediate combined plume is lazy. The same result follows from : enlarging the radius at fixed increases this parameter.
At fixed , the radius required for pure plume balance is
That is half the stipulated combined area . This fixed-speed pure-plume merger and flux conservation comparison exposes the limitation of demanding immediate pure balance with unchanged speed and reduced gravity: reducing the area to this value would also halve all three merged fluxes. A conservative merger must instead adjust its properties and begin out of pure balance. Under the given constant-entrainment equations, the resulting lazy plume subsequently approaches the attracting similarity solution with total buoyancy flux .