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The result is not much different from the conventional
decomposition into passive and active components
analyzed in Chapter 4, although the models are completely
different. Remember that, indeed,
uu u
=+
A
P
() () ()
2
(
)
(
)
uy euy u yuy e
τ
+
2
+
,
=
+
2
+
2
+
+
+
+
2
+
,
A
A
P
τ
if we assume, as does Panton [PAN 07], that t he o ver all
mean of the active and passive components and
is
not necessarily null. Indeed, we can see that the turbulent
intensity of the streamwise velocity is a superposition of two
functions, which are, respectively, dependent on and
independent of the Reynolds number.
uu
=−
A
P
The fundamental question remaining to be answered is
the extent to which the modulation caused by the large-scale
structures affects the Reynolds shear stress uv +
. In light of
equation [6.4], we can write
+
++
*
++
+
+
*
++ +
[6.8]
−≡− =−
uv
u v
u v
α
u
v
β
u v u
p
OM
OM
where a triple correlation term resulting from the
modulation is clearly visible on the right-hand side. At
present, there are no experimental measured data and/or
DNS available evaluating the contribution of each term on
the right-hand side of equation [6.8], to our knowledge. It
does not seem completely illogical to attribute the role of
Townsend's active and passive structures, respectively, to
u
*
and
. If this hypothesis is correct, the contribution of
u
OM
to uv +
would be negligible because of the
dissimilarity of scales between the fluctuations in wall-
normal velocity which are essentially governed by local
structures and the large-scale velocity O u coming from the
center of the logarithmic zone. The dissimilarity should
logically be more persistent between the fluctuations
O u ++
uv
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