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
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