Past exam of the mathematics course of the University of Cambridge 2019 iii Paper 345 3 a Solution Created 2026-10-03 Updated 2026-10-05
Take inward fluid entrainment speed to be positive. The non-Boussinesq form of the Batchelor entrainment hypothesis iswhere is the entrainment coefficient. Define physical, cross-section-integrated fluxes for the top-hat plume model byThus is mass flux, is momentum flux, and is a density-weighted buoyancy flux. The kinematic buoyancy flux in the Boussinesq approximation is . These definitions keep the factor ; conventions suppressing it simply rescale all three fluxes consistently.
For a homogeneous ambient, the sectional volume, mass and momentum balances areThe momentum source is the net upward buoyancy force; entrained ambient fluid initially supplies no vertical momentum. Subtracting the mass balance from times the volume balance gives conservation of the density deficit:Now , , and . Substitution produces the non-Boussinesq top-hat plume equationsFor reconstructing the fields without a Boussinesq approximation,The last expression uses the plume density in the acceleration denominator; it agrees with the ambient-density definition of reduced gravity to Boussinesq order.
Past exam of the mathematics course of the University of Cambridge 2019 iii Paper 345 3 b Solution Created 2026-10-03 Updated 2026-10-05
Use the kinematic fluxes , and . In the steady Boussinesq approximation, the non-Boussinesq top-hat plume equations reduce toEliminating gives , where the integration constant vanishes for a pure plume from a point source. Write and . The two balances give and . The Boussinesq point-source plume is thereforeHere and tend to zero at the source, while remains positive. The plume Froude number is independent of height:The ideal point source is a far-field similarity idealization. Since , the Boussinesq approximation fails near and is valid only when . In terms of , this requires ; the density formula must not be extrapolated into its unphysical negative-density region.