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coordinate axes, in which case the expression of the
dissipation is
2
2
2
= ν
u k
u k
u
v
w
*
ε K hom
x i =
2
ν
+
+
+
x i
x
y
z
[2.41]
2
2
2
2
2
2
u
v
u
w
v
w
+
ν
+
+
+
+
+
y
x
z
x
z
y
It is easy to show that the homogeneous enstrophy is
directly linked to
(
)
*
[2.42]
ωω
=
νε
i
i
K hom
hom
Using DNS in a channel with a low Reynolds number,
[ANT 91] showed that local homogeneity is an acceptable
hypothesis in wall turbulence for the case of dissipation, and
that
≈ ε K ho * constitutes a good approximation. In light of
equation [2.51], the ratio
ε *
i + /
*
+ is near to 1 throughout
ω
ω
ε
i
K
the channel (Figure 2.9)
*
ε *
Figure 2.9. Distribution of a)
and b)
ε
in a turbulent channel flow
Re=180
(solid line) and 360 (dotted line) according to [ANT 91].
The ratio of the enstrophy to the dissipation in inner variables is near to
1 c). This figure is adapted from [ANT 91]
K hom
when
τ
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