Environmental Engineering Reference
In-Depth Information
de
nition of new velocity variables that can be identi
ed distinctly with the base
fl
flow and the acoustics. The time-averaging over the slower of the two time scales
formally ensures that the slower process would pose to be rate-limiting in the
coupling between the two, and that the evolution of the coupled system would
occur at the slower time scale only. The averaging also results in the appearance of
explicit interaction terms between the base-
fl
ow and acoustics. The
final sets of
conservation equations for the
fl
flow and acoustics are given below (Chakravarthy
et al. 2007 ).
Flow:
¼
@q 0
@ t þ @
q 0 u 0j s
0
ð
1
Þ
@ x j
þ
@q 2
@ x i
@
@ t
Þþ @
@ x j
1
c
q 0 u 0i s
q 0 u 0i s u 0j s
ð
!
ð
2
Þ
u 0i s
@ x
2
@ u 0k s
@ x k
1
Re
@
1
3
@
@ x i
¼ @
@ x j
s
q 0 u 0 0i u 0 0j
þ
2
j
dt þ cq 0 @ u 0 j s
2
d q 0
c
Pe
@
T 0
@ x
@ x j ¼ðc
1
Þ Da Q R0 þ
ð
3
Þ
2
j
2
@q K 0
@ t
þ @
@ x j
1
ReSc
@
q K0
@ x
q K0 u 0j s
Da K x K ¼
0
ð
4
Þ
2
i
p 0 ¼ q 0 T 0
ð
5
Þ
Acoustics:
@q 1
@s þ @
¼ @
@n j
þ q 0 0 u 0j s 0 x x
q 0 x u 0j s x
q 0 x u 0 0j
ð
6
Þ
@n j
q 0 x @ u 0 0 i
1
c
@ p 1
@n i ¼
@s þ
0
ð
7
Þ
@n i ¼c p 0 @ u 0 j s x
@s þ c p 0 @ u 0 0 j
@ p 1
ð
8
Þ
@n i
@q K 1 x
@s
þ @
@n i
q K0 x u 0 0j
ð
9
Þ
¼ @
@n i
þ q 0 K0 u 0j s 0 x x
q K0 x u 0j s x
p 1 ¼ q 1 T 0 x
þ q 0 x T 1
ð
10
Þ
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