When a nonzero gravity field and temperature gradient are present simultaneously, the
-
models in Ansys Fluent can account for the generation of
due to buoyancy (
in Equation 4–39, Equation 4–42, and Equation 4–53), and the corresponding contribution to
the production of
in Equation 4–40, Equation 4–43,
and Equation 4–54.
The generation of turbulence due to buoyancy is given by
(4–64) |
where is the turbulent Prandtl number for energy and
is the component of the gravitational vector in the
th direction. For the standard and realizable
-
models, the default value of
is 0.85. For non-premixed and partially premixed combustion models,
is set equal to the PDF Schmidt number to ensure a Lewis number equal to unity.
In the case of the RNG
-
model,
=
, where
is given by Equation 4–47, but with
. The coefficient of thermal expansion,
, is defined as
(4–65) |
For ideal gases, Equation 4–64 reduces to
(4–66) |
It can be seen from the transport equations for (Equation 4–39, Equation 4–42, and
Equation 4–53) that turbulence kinetic energy tends to be
augmented (
) in unstable stratification. For stable stratification, buoyancy tends to
suppress the turbulence (
). In Ansys Fluent, the effects of buoyancy on the generation of
are included by default when you have both a nonzero gravity field and a
nonzero temperature (or density) gradient.
While the buoyancy effects on the generation of are relatively well understood, the effect on
is less clear. In Ansys Fluent, by default, the buoyancy effects on
are neglected simply by setting
to zero in the transport equation for
(Equation 4–40, Equation 4–43, or
Equation 4–54).
However, you can include the buoyancy effects on in the Viscous Model Dialog Box. In this
case, the value of
given by Equation 4–66 is used in the transport equation
for
(Equation 4–40, Equation 4–43, or
Equation 4–54).
The degree to which is affected by the buoyancy is determined by the constant
. In Ansys Fluent,
is not specified, but is instead calculated according to the following
relation [238]:
(4–67) |
where is the component of the flow velocity parallel to the gravitational vector and
is the component of the flow velocity perpendicular to the gravitational
vector. In this way,
will become 1 for buoyant shear layers for which the main flow direction is
aligned with the direction of gravity. For buoyant shear layers that are perpendicular to the
gravitational vector,
will become zero.