2012
DOI: 10.1007/s10494-012-9390-3
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Exploring k and ϵ with R–Equation Model Using Elliptic Relaxation Function

Abstract: An extended version of the isotropic R-equation model accompanied by an elliptic relaxation approach to account for the distinct effects of low-Reynolds number (LRN) and wall proximity is proposed. The turbulent kinetic energy k and the dissipation rate are evaluated using the R (= k 2 /˜ ) transport equation together with some empirical relations. The eddy viscosity formulation maintains the positivity of normal Reynolds stresses and the Schwarz' inequality for turbulent shear stresses. The model coefficients… Show more

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Cited by 30 publications
(11 citation statements)
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“…In the past several decades, considerable research has been devoted to improving the accuracy of one-equation models, for both equilibrium and nonequilibrium flows [2][3][4][5][6][7][8][9]. The Baldwin-Barth (BB) model [2] derived using the k-ϵ closure is one of the first oneequation models that does not explicitly use the algebraic length scales.…”
mentioning
confidence: 99%
“…In the past several decades, considerable research has been devoted to improving the accuracy of one-equation models, for both equilibrium and nonequilibrium flows [2][3][4][5][6][7][8][9]. The Baldwin-Barth (BB) model [2] derived using the k-ϵ closure is one of the first oneequation models that does not explicitly use the algebraic length scales.…”
mentioning
confidence: 99%
“…1 Concerning the complexity of calculation and increased cost, a non-linear one-equation turbulence model can provide solutions of similar and sometimes better predictive accuracy than the conventional two-equation models . [2][3][4][5][6] However, one-equation RANS (Reynolds-averaged Navier-Stokes) turbulence models that use a geometrically prescribed turbulent length scale have often shown limited success . 7 Therefore, accurate evaluations of velocity and length scales are required in turbulence modeling that are obtained from the transport equation of turbulent kinetic energy k and an algebraic length-scale determining quantity such as the dissipation ǫ or the specific dissipation ω.…”
Section: Introductionmentioning
confidence: 99%
“…The motivation for this approach is that the BB model is constrained by assumptions inherited from the k-ǫ model. Recently, Rahman et al 9,10 have devised new models, called the RAS and Rahman-Wallin-Siikonen models that address the weakness of BB model and account for the non-equilibrium and anisotropic effects, a feature that is missing in the single-equation models developed so far.…”
Section: Introductionmentioning
confidence: 99%