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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