For a turbulent plume in a homogeneous ambient of density , define actual sectional mass flux, momentum flux and density-weighted buoyancy flux by , and . With non-Boussinesq Batchelor entrainment , their balances areHere is sectional mass, is sectional density-deficit buoyancy, and the entrained ambient initially has zero vertical momentum. The last equation follows by subtracting mass conservation from times volume conservation. Scase, Caulfield, Dalziel and Hunt's time-dependent plume model derives the equivalent system with the common factor suppressed.
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