Civil Engineering Reference
In-Depth Information
By combining equations [2.12], [2.13] and [2.14], we are
able to write
⎛
⎞
π
i
*
2
b
ij
−
db
ij
dt
*
[2.15]
⎜
⎟
=−
2
b
ij
−
1
⎜
⎟
⎝
⎠
*
, the
tensor
b
ij
returns to isotropy. The simplest way of modeling
π
i
*
is then to consider that
Suppose that under the influence of the term
π
ij
b
ij
, in which case the term in
parentheses on the right of equation [2.15] is a constant
C
and the tensor
b
i
*
becomes isotropic with long times, because
b
i
*
π
i
*
∝
e
−
Ct
*
. The constant
C
must be positive,
and therefore the constant
C
R
in
0
when
t
*
→∞
=
→
2
C
R
b
ij
must be
greater than 1. To simplify this further, suppose that the
dissipation is isotropic, with
π
i
*
∝
b
ij
=−
∂
u
∂
u
2
3
ε
j
*
δ
ij
i
2
ν
l
=
∂
x
∂
x
l
By adding the condition of linear return to isotropy
π
i
*
C
R
b
ij
and rearranging equation [2.13], we find
∝
b
ij
=
⎛
⎞
⎛
⎝
⎞
⎠
∂
u
j
u
i
u
j
K
2
δ
1
ρ
x
i
+
∂
u
i
C
R
∂
u
i
∂
u
i
*
b
ij
ij
3
⎜
⎟
[2.16]
p
⎜
⎟
=−
2
C
R
ε
=−
−
∂
∂
x
j
∂
x
l
∂
x
l
⎝
⎠
Equation [2.16] is the original form of the model of return
to isotropy suggested by Rotta [ROT 51].
Choi and Lumley
[CHO 01] hypothesized that in
homogeneous turbulence, the tensor of return to isotropy
π
i
*
defined by equation [2.13] is symmetrical and depends solely
on the anisotropy tensor
b
ij
and the Reynolds number. Using
the invariant-based approach, we thus obtain the expression
*
a
0
b
i
0
a
1
b
i
1
a
2
b
i
2
[2.17]
π
=
+
+
ij
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