Reynolds Stress Transport Equation

The transport equation for the Reynolds stress tensor R is:

Figure 1. EQUATION_DISPLAY
t(ρR)+∇⋅(ρRv¯)=∇⋅D+P+G-23IϒM+_ϕρε̲+SR
(1309)

where:

For the Linear Pressure Strain and Quadratic Pressure Strain models, the dissipation is simply:
ε̲=23εI
(1310)

Seven equations must be solved (as opposed to the two equations of a K-Epsilon or a K-Omega model): six equations for the Reynolds stresses (symmetric tensor) and one equation for the isotropic turbulent dissipation ε (see Eqn. (1169) (SKE)).

Reynolds Stress Diffusion

Two different models for the Reynolds-stress diffusion are available. By default, following [343], a simple isotropic form of the turbulent diffusion is adopted, such that:

Figure 2. EQUATION_DISPLAY
D=(μ+μtσk)R
(1311)

where:

The turbulent viscosity μt is computed as:

Figure 3. EQUATION_DISPLAY
μ t = ρ C μ k 2 ε
(1312)

where Cμ is a Model Coefficient. The turbulent kinetic energy k is defined as:

Figure 4. EQUATION_DISPLAY
k=12tr(R)
(1313)

where tr(R) is the trace of the Reynolds stress tensor (see Eqn. (1146)).

Alternatively, the Reynolds-stress diffusion can be written according to Daly and Harlow [338] in the form:

Figure 5. EQUATION_DISPLAY
D=μR+Cskε(R)R
(1314)

where Cs is a Model Coefficient.

This model is also known as the Generalized Gradient Diffusion Hypothesis, GGDH.

Turbulent Production

The turbulent production is obtained directly, without recourse to modeling as follows:

Figure 6. EQUATION_DISPLAY
P=-ρ(Rv¯T+v¯RT)=-ρ(Rv¯T+v¯R)
(1315)

Buoyancy Production

For constant-density flows using the Boussinesq approximation, the buoyancy production is modeled as:

Figure 7. EQUATION_DISPLAY
G=β μtPrt(T¯g + gT¯)
(1316)

where:

  • β   is the coefficient of thermal expansion.
  • g is the gravitational vector.
  • Prt is the turbulent Prandtl number.
  • T¯ is the mean temperature.

For flows with varying density:

Figure 8. EQUATION_DISPLAY
G=μtρPrt(ρg + gρ)
(1317)

Turbulent Dissipation Rate

The isotropic turbulent dissipation rate is obtained from a transport equation analogous to the K-Epsilon model (and with identical boundary conditions):

Figure 9. EQUATION_DISPLAY
t(ρε)+∇⋅(ρεv¯)=∇⋅[(μ+μtσε)ε]+εk[Cε1(12tr(P)+12Cε3tr(G))-Cε2ρε]
(1318)

where:

Dilatation Dissipation Rate

The dilatation dissipation ϒ M is modeled as in the K-Epsilon model, using the model of Sarkar et al. [344]:

Figure 10. EQUATION_DISPLAY
ϒM=ρCMkεc2
(1319)

where:

Model Coefficients

Coefficient Linear Pressure Strain Linear Pressure Strain Two Layer Quadratic Pressure Strain Elliptic Blending
σk 1 0.82 1 1
σε 1.22 1 1.22 1.15
CM (Sarkar) 2 2 2 2
Cs 0.2 0.2 0.2 0.21
C ε 1 1.44 1.44 1.44 1.44
C ε 2 1.92 1.92 1.83 1.83
Cμ 0.065536 0.09 0.098596 0.07