One of the most important features of high Reynolds number turbulent flows is their large range of both space and time scales. The size of eddies in high Reynolds number, turbulent flows range from the energy - containing eddies of size L, the integral scale, down to the dissipation-scale eddies of size L/R3/4, where R is a microscale Reynolds number. To accurately solve the three dimensional Navier-Stokes equation for such a turbulent flow would require storage of order O(R9/4). As the time scale of turbulent eddies is of order O(R3/4) the amount of computational work is order O(R3). If R is large both the number of operations and the storage requirements are prohibitively large.
High Reynolds number, turbulent flow can be characterised by three ranges of spatial scales
| (25.28) |
The range of scales of the effective excitation in turbulence lie
between the low, energy containing wavenumber k0 = 2
and
the high wavenumber viscous cutoff
.
The RNG method removes
a narrow band of modes near
by expressing them in terms
of lower modes in the range
.
Having
removed this band of modes the equations of motions for the remaining
modes is a modified system of Navier-Stokes equations in which the
eddy viscosity, force and non-linear coupling have all been affected.
In turn, further modes are iteratively removed from the dynamics.
Thus the RNG method produces a form of the Navier-Stokes equation
which allows the computation on coarser grids.
The current implementation of the RNG model uses the same
equation as the standard k-e model for the turbulent
viscosity with the exception that the constant
has an adjusted value. A comparison of the values of a
number of constants used in the standard and RNG variants
of the k-e model are presented in the table below.
| |t:===:t| | Standard k-e | RNG k-e |
| ||-|-|-||
C
|
1.44 | 1.42 |
| ||-|-|-||
C
|
1.92 | 1.68 |
| ||-|-|-||
|
1.0 | 0.7194 |
| ||-|-|-||
|
1.314 | 0.7194 |
| ||-|-|-||
C |
0.09 | 0.0845 |
| |b:===:b| |
In addition to the above changes in the values of the constants
there is an extra source term in the dissipation rate equation which now
becomes