Two-equation model with superior near-wall treatment and boundary layer accuracy
The k-ω turbulence model was developed by David C. Wilcox in 1988 as an alternative to k-ε models, specifically designed to provide superior near-wall treatment and boundary layer prediction without the need for wall functions.
Wilcox's development of the k-ω model began in the 1980s with the recognition that k-ε models had fundamental limitations in the near-wall region. The original 1988 formulation introduced the specific dissipation rate ω as an alternative to the dissipation rate ε, providing better scaling properties near solid boundaries.
The 1998 revision (Wilcox k-ω '98) incorporated stress limiter functions and improved the model's performance in adverse pressure gradients. The 2006 version (Wilcox k-ω '06) further refined the model constants and addressed issues with separated flows. Despite being superseded by SST variants for many applications, the original k-ω model remains important for educational purposes and specific boundary layer applications.
The k-ω model solves two transport equations for turbulent kinetic energy (k) and specific dissipation rate (ω), providing closure for the Reynolds-averaged Navier-Stokes equations through the eddy viscosity hypothesis.
Constant | Value (1988) | Value (2006) | Physical Significance |
---|---|---|---|
β* | 0.09 | 0.09 | Dissipation coefficient |
α | 5/9 | 0.52 | Production coefficient |
β | 0.075 | 0.0708 | ω destruction coefficient |
σₖ | 2.0 | 0.6 | Turbulent Prandtl number for k |
σ_ω | 2.0 | 0.5 | Turbulent Prandtl number for ω |
The k-ω model represents a fundamental advance in turbulence modeling by using the specific dissipation rate ω instead of the dissipation rate ε, providing superior behavior in the near-wall region and boundary layers.
The variable ω = ε/(β*k) represents the frequency of the energy-containing turbulent eddies. This formulation provides better scaling properties near walls compared to ε-based models, eliminating the need for wall functions in many applications.
The k-ω formulation naturally integrates to the wall with boundary conditions k = 0 and ω = 6ν/(β₁y₁²) where y₁ is the distance to the first grid point. This provides superior boundary layer prediction without complex wall function treatments.
The turbulent length scale in k-ω models is defined as l_t = √k/ω, which provides appropriate scaling near walls and in boundary layers. This contrasts with k-ε models where the length scale k^(3/2)/ε becomes problematic near solid boundaries.
Unlike k-ε models that require wall functions or complex low-Reynolds number modifications, the k-ω model can integrate directly to the wall surface with proper boundary conditions, making it particularly suitable for boundary layer applications.
While the k-ω model provides excellent near-wall behavior, it suffers from significant limitations that have led to the development of improved variants like SST.
The primary limitation of the k-ω model is its excessive sensitivity to inlet boundary conditions for ω in the freestream. Small changes in the specified ω values can dramatically affect the solution, particularly in external flows.
The k-ω model generally under-predicts spreading rates in free shear flows such as:
The original k-ω model tends to predict separation too early in adverse pressure gradients, particularly on smooth surfaces like airfoils at moderate angles of attack.
The k-ω model has been extensively validated for specific flow types where its strengths can be utilized while avoiding its known limitations.
Standard validation includes flat plate boundary layers, Falkner-Skan flows, pipe and channel flows, and simple separated flows. The model generally shows excellent agreement for attached boundary layers but struggles with external flows and complex separation.
While superseded by SST for most engineering applications, the k-ω model remains valuable for:
The k-ω model has undergone several revisions and has served as the foundation for numerous advanced turbulence models.
Original 1988 model established the basic k-ω framework with simple constant formulation. The 1998 revision introduced stress limiter functions and improved constants. The 2006 version (k-ω '06) incorporated cross-diffusion terms and addressed freestream sensitivity issues to some extent.
Several low-Reynolds number modifications have been developed to improve near-wall behavior and handle transitional flows. These variants include damping functions and modified source terms for very low Reynolds number applications.
The k-ω model served as the foundation for several important developments:
Successful implementation of the k-ω model requires careful attention to boundary conditions, mesh requirements, and numerical considerations.
Proper boundary condition specification is critical for k-ω model success:
The k-ω model's direct wall integration capability requires specific mesh considerations:
The k-ω model generally provides good convergence characteristics, but optimization includes appropriate under-relaxation factors (typically k: 0.6, ω: 0.6), monitoring of both residuals and integral quantities, and careful initialization procedures especially for ω boundary conditions.