Civil Engineering Reference
In-Depth Information
Let us first consider Figure 2.2
9,
which shows the
evolution of the structural parameter
uv
2
K
as a function of
−
, o
n the basis of data taken from [MAX 82]. We can see that
α
uv
2
K
first increases in an almost linear fashion with
increasing strain, then reaches a local maximum
bef
ore
beginning to fall off. Figure 2.30 shows the profiles
−
uv
2
K
−
stemming from the closure
k
-
with and w
it
hout viscous
damping near to the wall. The maximum
ω
uv
2
K
attained
corresponds, in both cases, to the response of an
axisymmetrical
−
turbulence
whose
initial
anisotropy
parameter is
s
1.2
(Figure 2.29). The strain is null at the
center of a channel, and increases as we approach the wall. A
correspondence can thus be establi
sh
ed by determining the
distribution
=
()
uv
2
K
at a given position
y
+
with the results found by the RDT. The effective
strain
+
, which links
α
y
−
eff
()
+
is qualitatively linked to the distortion of an
initially homogeneous and axisymmetrical turbulence whose
evolution was halted by the nonlinearity and which,
therefore, led to an equilibrium distribution.
α
y
eff
Figure 2.30.
Profile of Reynolds shear stress generated by the closure
k
Re = 440
. The solid line corresponds to the
profile obtained without taking viscous damping into account; the crosses
indicate the results arising from standard
k
in a channel where
− ω
τ
with viscous damping.
This figure is adapted from [TAR 05]
− ω
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