Abstract
A previous formulation of plume merger [Rooney, J. Fluid Mech. 796, 712 (2016)] is generalized to model both Boussinesq and non-Boussinesq plume rise in a corner of arbitrary angle where . The Boussinesq plume theory predicts the correct near- and far-field similarity solutions when is noninteger. Moreover, an alternate entrainment assumption is proposed whereby the rate of entrainment per unit height correlates directly to the plume perimeter. Model predictions made using this alternative entrainment assumption agree well with a previous prediction for the plume volume flux when . For non-Boussinesq plumes, the theory also approaches the correct near- and far-field similarity limits. When the source area is compact, and regardless of the corner angle, the non-Boussinesq height, i.e., height over which non-Boussinesq effects are important, is small compared to the contact height between the plume and the corner. When the source area is relatively large, the non-Boussinesq height can be comparable to the contact height; enhanced non-Boussinesq effects are observed for smaller corner angles. Our Boussinesq theory is adapted to the natural ventilation model developed by Linden et al. [J. Fluid Mech. 212, 309 (1990)] and agrees well with previous experimental and theoretical predictions for the steady-state depth of the layer of discharged plume fluid that accumulates along the ceiling of the (ventilated) interior space. For non-Boussinesq plumes, the counterpart theory compares satisfactorily with previously measured results of fire plume mass flux.
8 More- Received 12 February 2021
- Accepted 4 May 2021
DOI:https://doi.org/10.1103/PhysRevFluids.6.054503
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