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The Wilcox k-omega Turbulence Model
This web page gives detailed information on the equations for various forms of the Wilcox k-omega turbulence model. If any particular variant has been overlooked, please report it to the page curator.
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Wilcox (2006) k-omega Two-Equation Model (Wilcox2006)
The references for this model are:
The two-equation model (written in conservation form) is given by the following:
![\frac{\partial (\rho k)}{\partial t} + \frac{\partial (\rho u_j k)}{\partial x_j}
= \cal P - \beta^* \rho \omega k + \frac{\partial}{\partial x_j}
\left[\left(\mu + \sigma_k \frac{\rho k}{\omega} \right)\frac{\partial k}{\partial x_j}\right]](wilcox2006_eqns/img2.png)
![\frac{\partial (\rho \omega)}{\partial t} + \frac{\partial (\rho u_j \omega)}{\partial x_j}
= \frac{\gamma \omega}{k} \cal P -
\beta \rho \omega^2 + \frac{\partial}{\partial x_j}
\left[ \left( \mu + \sigma_{\omega} \frac{\rho k}{\omega} \right)
\frac{\partial \omega}{\partial x_j} \right] +
\frac{\rho \sigma_d}{\omega} \frac{\partial k}{\partial x_j}
\frac{\partial \omega}{\partial x_j}](wilcox2006_eqns/img3.png)
where



and the turbulent eddy viscosity is computed from:

where:
![\hat \omega = {\rm max} \left[ \omega, C_{lim}
\sqrt{\frac{2 \overline S_{ij} \overline S_{ij}}{\beta^*}} \right]](wilcox2006_eqns/img8.png)

and
is the density
and
is the
molecular dynamic viscosity.
There are no specific farfield boundary conditions recommended for this model. See Menter k-omega SST for farfield values recommended there. At solid walls:

There are various wall boundary conditions mentioned for
in the references above, including both smooth and rough walls. For smooth walls, the
asymptotic behavior is

as
,
where d is the distance to the nearest wall.
The references also specify a so-called "slightly-rough-surface" boundary
condition for
:

where it is important for smooth walls to "select a small enough value" of
to insure that
.
Some CFD codes employ the approximate
wall boundary condition from Menter for this model
(see Menter k-omega SST).
The constants and auxiliary functions are:








Wilcox (1998) k-omega Two-Equation Model (Wilcox1998)
The reference for this model is:
The two-equation model (written in conservation form) is given by the following:
![\frac{\partial (\rho k)}{\partial t} + \frac{\partial (\rho u_j k)}{\partial x_j}
= \cal P - \beta^* \rho \omega k + \frac{\partial}{\partial x_j}
\left[\left(\mu + \sigma_k \frac{\rho k}{\omega} \right)\frac{\partial k}{\partial x_j}\right]](wilcox1998_eqns/img2.png)
![\frac{\partial (\rho \omega)}{\partial t} + \frac{\partial (\rho u_j \omega)}{\partial x_j}
= \frac{\gamma \omega}{k} \cal P -
\beta \rho \omega^2 + \frac{\partial}{\partial x_j}
\left[ \left( \mu + \sigma_{\omega} \frac{\rho k}{\omega} \right)
\frac{\partial \omega}{\partial x_j} \right]](wilcox1998_eqns/img3.png)
and the turbulent eddy viscosity is computed from:

Meanings of variables and definitions of boundary conditions are the same as for (Wilcox2006).
The constants and auxiliary functions are:








Wilcox (1988) k-omega Two-Equation Model (Wilcox1988)
The references for this model are:
The basic equations for this two-equation model are the same as for (Wilcox1998):
![\frac{\partial (\rho k)}{\partial t} + \frac{\partial (\rho u_j k)}{\partial x_j}
= \cal P - \beta^* \rho \omega k + \frac{\partial}{\partial x_j}
\left[\left(\mu + \sigma_k \frac{\rho k}{\omega} \right)\frac{\partial k}{\partial x_j}\right]](wilcox1988_eqns/img2.png)
![\frac{\partial (\rho \omega)}{\partial t} + \frac{\partial (\rho u_j \omega)}{\partial x_j}
= \frac{\gamma \omega}{k} \cal P -
\beta \rho \omega^2 + \frac{\partial}{\partial x_j}
\left[ \left( \mu + \sigma_{\omega} \frac{\rho k}{\omega} \right)
\frac{\partial \omega}{\partial x_j} \right]](wilcox1988_eqns/img3.png)
and the turbulent eddy viscosity is computed from:



Wilcox k-omega Two-Equation Models with Vorticity Source Term (Wilcox2006-V, Wilcox1998-V, Wilcox1988-V)
This form of two-equation models is sometimes used because vorticity magnitude
is usually readily available in
most Navier-Stokes codes. Furthermore, the vorticity source term is often nearly identical to the exact source
term in simple boundary layer flows, and the use of the vorticity term can avoid some numerical difficulties
sometimes associated with the use of the exact source term.
The reference for this usage is:
The equations are the same as for the "standard" versions of the Wilcox models, with the exception that the term P (in both equations) is approximated with the following:

For low-speed flows, the second term on the right hand side of this equation
is generally small compared to the first term. (For incompressible flows the second term is identically zero.)
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