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viscosity, govern the mechanism of turbulent transport in
both cases. Coles 8 proposed a velocity distribution that is
valid both in the logarithmic sublayer and the outer layer, by
adding a function known as a “wake function”, to the
distribution [1.25]:
1 ln
Π
y
()
Uy yB W
κ
++
=
+
+
+
,
Π
[1.43]
c
κ
Λ
0
where the argument of the wake function W is the distance
from the wall, rendered dimensionless by the external scale
Λ
(the half-height h of a channel or the thickness
of a
δ
0
boundary layer) and
is a constant that depends slightly
on the Reynolds number in a canonic boundary layer without
pressure gradient and varies between 0.54 and 0.55. The
empirical function
Π
W , proposed by Coles, is
(
)
21
1 in
η
π
()
[1.44]
W
η
=+
2
where
depends (slightly) on the
Reynolds number in a boundary layer without pressure
gradient and typically varies between 0.54 and 0.55.
η =Λ
y
. The constant
Π
0
Let us look again at the distribution [1.28] in outer scales.
Generally speaking, this distribution depends not only on the
variable
η
=Λ=
y
y
δ
, but also on the Reynolds number,
0
+
expressed as
δδν
=
u
τ
. Thus, relation [1.28] is expressed in
the general form:
()
UUy g
u τ
(
)
[1.45]
+
=
η δ
,
8 These results were published in the first edition of the Journal of Fluid
Mechanics (vol. 1, p. 191, 1956), a renowned journal in this field.
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