Seek a nonzero-buoyancy, separable similarity solution of the unsteady Boussinesq triangular-profile line-plume balances, using powers of distance and time. Let , allowing a time origin, and initially take distance from the virtual origin. Balancing the powers in the momentum and buoyancy equations and the entrainment balance gives the formOne way to recover the exponents is to let and . Matching the spatial powers in , and gives ; matching the time powers gives . The momentum equation then gives the powers of . In the resulting solution, is time-independent, so the storage term in the first equation vanishes exactly.
Direct substitution yields the coefficient equationsFor a rising buoyant solution , the last equation gives . The first then gives , and the second gives . The separable decaying line-plume similarity is thereforeReconstructing the physical fields confirmsFor example, and cancel; the momentum balance similarly gives .
The unshifted form uses and is defined for , with a singular zero-time limit. To give a finite solution for all , choose . The equations also permit replacing by , a plume virtual origin; at a finite physical source distance this family has flux histories proportional to . The Boussinesq approximation requires in the region modelled. This is a decaying similarity family; its time and virtual origins require source or initial data. The PDF supplies neither, so a unique forced-startup history cannot be selected from it. In particular, the singular unshifted field should not be presented as a regular solution at .
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