Civil Engineering Reference
In-Depth Information
where
U
,
V
and
W
are, respectively, the instantaneous
components of the velocity vector in directions
x y
and
z
,
and
P
is the (instantaneous) pressure. The final term
includes all the viscosity terms. This equation is valid at any
time
t
(with the appropriate initial and boundary
conditions). The instantaneous components of the velocity
vector
G
vary in time and space, while the flow, at
any given time, is highly unsteady and three-dimensional
(3D). If we look at the behavior of
u
ρ
over long periods, then
we need to average equation [1.10] over time. To do so, we
decompose each physical value
(
)
UUxt
=
,
i
i
Qx
ρ
into a temporal
(
)
,
Q
G
and a fluctuating value
()
(
G
)
average value
, where
qxt
,
.
Thus
we
have,
for
example,
q
=
0
(
)
(
)
UU U u U u UU uu
=+
+=
+
, and the correlation
i
j
i
i
j
j
i
j
i
j
between the fluctuations
uu
is generally non-null.
Equation [1.10], subjected to this treatment and
appropriately arranged, is written as
i
j
∂
U
∂
U
∂
U
1
∂
P
∂
uu
∂
uv
∂
uw
[1.11]
UV W U
x
+
+
= −
+
ν
∇
2
−
−
−
∂
∂
y
∂
z
ρ ∂
x
∂
x
∂
y
∂
z
and generally:
∂
uu
∂
U
1
∂
P
i
j
2
[1.12]
U
i
=−
+ ∇
ν
U
−
i
j
∂
x
ρ ∂
x
∂
x
j
i
j
The continuity equation, for its part, is of the same form
fo
r
the average field and the fluctuating field; in other words,
0
, with the latter identity being
valid instantaneously. What we need to take away from
these equations (and by comparison with a laminar flow) is
the existence of the t
erm
s of inter-correlation or cross-
correlation of the type
∂∂=
Ux
and
∂∂=
ux
0
i
i
i
i
uu
. These terms, called Reynolds
i
j
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