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When a non-zero gravity field and temperature gradient are present simultaneously, the
-
models in
ANSYS FLUENT account for the generation of
due to buoyancy (
in Equations
4.4-1,
4.4-4, and
4.4-15), and the corresponding contribution to the production of
in Equations
4.4-2,
4.4-5, and
4.4-16.
The generation of turbulence due to buoyancy is given by
where Pr
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 Pr
is 0.85. In the case of the RNG
-
model, Pr
=
, where
is given by Equation
4.4-9, but with
. The coefficient of thermal expansion,
, is defined as
For ideal gases, Equation 4.4-23 reduces to
It can be seen from the transport equations for
(Equations
4.4-1,
4.4-4, and
4.4-15) 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 always included when you have both a non-zero gravity field and a non-zero 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
4.4-2,
4.4-5, or
4.4-16).
However, you can include the buoyancy effects on
in the
Viscous Model dialog box. In this case, the value of
given by Equation
4.4-25 is used in the transport equation for
(Equation
4.4-2,
4.4-5, or
4.4-16).
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 [
127]:
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(4.4-26) |
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.