Civil Engineering Reference
In-Depth Information
Indeed, the production and advection terms disappear in
the ab sence of mean velocity, and all the terms such as
∂∂
()
are zero for reasons of homogeneity. For
homogeneous, isotropic turbulence, u i u j
x i
3 . The
=
u k u k
δ
ij
transport equation is then
u i u j
2
3 ε
*
δ ij
[2.11]
=−
t
where the isotropic dissipation rate is
x j . By
rearranging equations [2.10] and [2.11], we find a formal
relation
*
ε
= ∂
u i
x j
u i
u
i u
u
u
1
ρ
i +
u i
u i
2
3 ε
2
3 ε
j
j
j
*
*
δ ij [2.12]
=
p
2
ν
l +
δ ij
t
x
x
x
x
j
l
The term in square brackets in equation [2.12] is clearly
responsible for the return to isotropy. Let us introduce the
modified
tensor
of
the
pressure/velocity
gradient
correlations, defined by
u
u
1
u
u
2
**
j
j
*
[2.13]
επ
=
p
+
i
2
ν
i
+
εδ
ij
ij
ρ∂ ∂
x
x
∂∂
x
x
3
i
j
l
l
Let us also introduce the anisotropy tensor, which we will
return to later on in this chapter:
uu
K δ
i
j
ij
b
=−
[2.14]
ij
2
3
In this relation, K
u i u i 2 is the kinetic energy. Note that
=
0 for homogeneous isotropic turbulence. Let us also
introduce a time scale
b ij
*
ε
dt *
dt
=
2 K
Search WWH ::




Custom Search