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can be engendered because of the spanwise symmetry
(in direction
z
). Indeed, the value of
wx
∂∂
wx
is:
∂∂
∞∞ ∞
∂
w
1
∫∫∫
[5.107]
(, ,,)
x y z t
=−
(
x
−
x
)
F dx dy dz
' ' '
∂
x
4
π
−∞
−∞
z
'0
=
where, in light of equation [5.106]
∂
∂
ω
y
+
x
'
F
=
⎡
3/2
(
) (
2
)
2
(
)
2
⎤
xx
−+− ++
'
yy
'
zz
'
⎣
⎦
[5.108]
∂
∂
ω
y
−
x
'
−
⎡
3/ 2
(
)
(
)
(
)
⎤
2
2
2
xx
−+−+−
'
yy
'
zz
'
⎣
⎦
Thus, if spatially and temporally,
,
∂ω
∂
x
'
=
∂ω
∂
x
'
y
+
y
−
then
will be null in the zone in question. The creation
∂∂
wx
of
∂∂
wx
depends
directly
on
the
difference
. We can show
this rigorously by averaging equation [5.107] at a given
distance
y
across a surface
S
which is axisymmetrical in the
plane
x
Δ
( , , ,)
x
yzt
=
∂ω
∂
x
'
−
∂ω
∂
x
'
y
+
y
−
−
z
(Figure 5.45). The mean value of
across
∂∂
wx
S
is then:
∂
w
1
∫∫
=−
GdxdydzdS
Δ
'
'
'
∂
x
4
π
S
SR
where
⎡
1
⎤
⎢
⎥
3/2
⎡
(
) (
2
)
2
(
)
2
⎤
xx
−+− ++
'
yy
'
zz
'
⎢
⎥
⎣
⎦
⎢
⎥
Gxx
=−
⎢
(
')
1
⎥
−
⎢
⎥
3/2
⎡
(
) (
)
(
)
⎤
2
2
2
⎢
xx
−+− +−
'
yy
'
zz
'
⎥
⎣
⎦
⎣
⎦
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