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contributor authorMichael A. Delichatsios
contributor authorC. P. Brescianini
contributor authorH. Y. Wang
contributor authorJ. M. Most
contributor authorD. Paterson
date accessioned2017-05-09T00:38:14Z
date available2017-05-09T00:38:14Z
date copyrightJune, 2010
date issued2010
identifier issn0098-2202
identifier otherJFEGA4-27421#061202_1.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/143470
description abstractComputational fluid dynamics based on Reynolds averaged Navier–Stokes equations is used to model a turbulent planar buoyant adiabatic wall plume. The plume is generated by directing a helium/air source upwards at the base of the wall. Far from the source, the resulting plume becomes self-similar to a good approximation. Several turbulence models based predominantly on the k-ε modeling technique, including algebraic stress modeling, are examined and evaluated against experimental data for the mean mixture fraction, the mixture fraction fluctuations, the mean velocity, and the Reynolds shear stress. Several versions of the k-ε model are identified that can predict important flow quantities with reasonable accuracy. Some new results are presented for the variation in a mixing function for the mixture normal to the wall. Finally, the predicted (velocity) lateral spread is as expected smaller for wall flows in comparison to the free flows, but quite importantly, it depends on the wall boundary conditions in agreement with experiments, i.e., it is larger for adiabatic than for hot wall plumes.
publisherThe American Society of Mechanical Engineers (ASME)
titleApplication of the k-ε Turbulence Model to Buoyant Adiabatic Wall Plumes
typeJournal Paper
journal volume132
journal issue6
journal titleJournal of Fluids Engineering
identifier doi10.1115/1.4001642
journal fristpage61202
identifier eissn1528-901X
keywordsFlow (Dynamics)
keywordsTurbulence
keywordsPlumes (Fluid dynamics)
keywordsMixtures AND Fluctuations (Physics)
treeJournal of Fluids Engineering:;2010:;volume( 132 ):;issue: 006
contenttypeFulltext


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