Batchelor entrainment models a turbulent plume as drawing ambient fluid inward at a speed proportional to its characteristic vertical velocity. In a top-hat axisymmetric plume, letbe volume, momentum, and buoyancy flux. The Boussinesq approximation uses a common density in inertia and volume conservation while retaining the small density difference in . It requires and becomes inaccurate for very hot source fluid or near openings with large density changes.
For a point source in an unstratified lower layer, the integral plume equations arewhere is the entrainment coefficient. Their pure-plume solution iswith
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