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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