Civil Engineering Reference
In-Depth Information
. The wall-normal vorticity layer becomes
approximately streamwise a little later on. It behaves like a
Burgers vortex, subjected to ux
δ
l
ς
t
x
ω
and v
, where the
=
β
=−
β
y
1
d
dt
δ
1
strain rate is
β
=−
=
. The 2D spatiotemporal
δ
t
development which governs the regeneration of
ω
is then
x
2
∂ω
∂ω
ω
∂ ω
y
x
x
x
x
[5.54]
=
+
ν
t
t
y
t
y
2
This equation can have a self-similar solution, of the form
(
)
ω
t
1/ 2
exp
3
y
2
4
ν
t
x
The viscosity governs the thickness
at long times for
δ
and
which
. The behaviors for short times
δ
2
ν
t
δ
l
ξ
t
x
ω
(
)
1/3
*
2
2
long times
δ
2
ν
t
coincide at time
t
l ω
4
νξ
. The
x
vorticity reaches its peak at
tt
=
*
and the thickness
(
)
1/ 3
reaches its minimum.
δ
*
2
ν
t
*
=
4
l
ν ξ
x
ω
Jiménez [JIM 94] assumes that the origin of the wall-
normal vorticity layer
is the instability of the streaks.
These are represented schematically as two coflowing plane
jets (high- and low-velocity streaks), at a distance
ω
y
apart.
The most unstable linear mode of a jet is sinuous 18 with a
wavelength 2.5 times greater than the thickness of the jet
2
λ
is half of the most unstable
wavelength, i.e. combining
. The thickness
λ
l ω
. Each streak engenders
two vorticity layers of opposite signs. These layers roll up
into counter-rotating vortices, if they are sufficiently intense.
l ω
=
58
λ
18 However, it should be noted that the streaks are mainly linearly stable
in the inner layer. We will return to look at this point in detail later on in
this chapter.
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