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Flows completely bounded by solid surfaces are called internal flows. External flows are flows over bodies immersed in an unbounded fluid[ 1] .
Internal flows might be laminar or turbulent. The state of the flow regime is dependent on Re(Reynold Number). There might be an analytical solution for laminar flows but not for turbulent flows.
Flows through pipes, ducts, nozzles, diffusers, valves and fittings are examples of internal flows.
Flow around an airplane is an example of an external flow.
Flow around a car is classified under external flows.
Velocity profiles for laminar (upper) and turbulent (lower) states at the same mass flow rate
At fully developed state the velocity profile becomes parabolic for laminar flow. The average velocity at any cross section is:
U
¯
=
U
0
=
V
=
1
A
∫
A
r
e
a
U
1
d
A
{\displaystyle {\bar {U}}=U_{0}=V={\frac {1}{A}}\int _{Area}{U_{1}dA}}
For the same flow value i.e.
U
0
{\displaystyle U_{0}}
, the fully developed turbulent pipe flow, would have higher velocity close to the wall and lower velocity at the center. The reason is the turbulent eddies, which causes more momentum loss to the wall i.e. higher velocity gradients close to the wall. Note that such a direct comparison is only valid at the same
R
e
=
U
0
D
ν
{\displaystyle Re={\frac {U_{0}D}{\nu }}}
.
Signal measured by a hot-wire at a center of a pipe during transition showing the development of transitional structures along the pipe at different Reynolds numbers[ 2] [ 3] and the change of friction coefficient at laminar, transitional and turbulent regimes.
Development of velocity profile in a pipe with increasing Reynolds number
Consider the flow in a channel between two plates having a height of
D
{\displaystyle D}
and an infinite depth in
x
3
{\displaystyle x_{3}}
direction.
Starting from the entrance, the boundary layers develop due to the no-slip condition on the wall.
At a finite distance, the boundary layers merge and the inviscid core (field with no velocity gradient in
x
2
{\displaystyle x_{2}}
direction) vanishes.
The flow becomes fully viscous. The velocity field in
x
1
{\displaystyle x_{1}}
direction adjusts slightly further until
x
1
=
L
e
{\displaystyle x_{1}=L_{e}}
and it no longer changes with
x
1
{\displaystyle x_{1}}
direction. This state of the flow is called fully-developed.
Flow between two plates
At the fully developed state:
∂
U
i
∂
x
1
=
0
→
∂
τ
i
j
∂
x
1
=
0
{\displaystyle {\frac {\partial U_{i}}{\partial x_{1}}}=0\rightarrow {\frac {\partial \tau _{ij}}{\partial x_{1}}}=0}
Because of the two-dimensional nature of the flow, no gradient of the velocity quantities in
x
3
{\displaystyle x_{3}}
direction is expected starting from the entrance.
U
3
=
0
,
∂
U
i
∂
x
3
=
0
,
∂
τ
i
j
∂
x
3
=
0
,
∂
P
∂
x
3
=
0
,
{\displaystyle U_{3}=0\ ,\ {\frac {\partial U_{i}}{\partial x_{3}}}=0\ ,\ {\frac {\partial \tau _{ij}}{\partial x_{3}}}=0\ ,\ {\frac {\partial P}{\partial x_{3}}}=0,}
U
2
=
U
3
=
0
{\displaystyle U_{2}=U_{3}=0}
Hence,
U
1
=
U
1
(
x
2
)
,
τ
i
j
=
τ
i
j
(
x
2
)
.
{\displaystyle U_{1}=U_{1}(x_{2})\ ,\ \tau _{ij}=\tau _{ij}(x_{2}).}
The entrance lengths for laminar pipe and channel flows are, respectively[ 4] :
L
e
p
i
p
e
D
=
[
(
0.619
)
1.6
+
(
0.0567
R
e
)
1.6
]
1
1.6
{\displaystyle {\frac {Le_{pipe}}{D}}=\left[(0.619)^{1.6}+(0.0567Re)^{1.6}\right]^{\frac {1}{1.6}}}
L
e
c
h
a
n
n
e
l
D
=
[
(
0.631
)
1.6
+
(
0.0442
R
e
)
1.6
]
1
1.6
{\displaystyle {\frac {Le_{channel}}{D}}=\left[(0.631)^{1.6}+(0.0442Re)^{1.6}\right]^{\frac {1}{1.6}}}
Fully Developed Laminar Flow Between Infinite Parallel Plates [ edit | edit source ]
Fully developed flow in a channel with an infinite depth
Consider the fully developed laminar flow between two infinite plates.
Consider the continuity equation and momentum equation in
x
1
{\displaystyle x_{1}}
direction for an incompressible steady flow between two infinite plates as shown.
Continuity Equation
∂
ρ
∂
t
⏟
=
0
+
∂
ρ
U
i
∂
x
i
=
0
⟶
ρ
=
c
s
t
.
∂
U
i
∂
x
i
=
0
{\displaystyle \underbrace {\frac {\partial \rho }{\partial t}} _{=0}+{\frac {\partial \rho U_{i}}{\partial x_{i}}}=0\ {\stackrel {\rho =cst.}{\longrightarrow }}\ {\frac {\partial U_{i}}{\partial x_{i}}}=0}
Since
∂
U
1
∂
x
1
=
0
{\displaystyle {\frac {\partial U_{1}}{\partial x_{1}}}=0}
,
∂
U
3
∂
x
3
=
0
→
∂
U
2
∂
x
2
=
0
{\displaystyle {\frac {\partial U_{3}}{\partial x_{3}}}=0\rightarrow {\frac {\partial U_{2}}{\partial x_{2}}}=0}
because it is a fully-developed and two dimensional flow. Hence,
U
2
{\displaystyle \ U_{2}}
reads
U
2
=
c
o
n
s
t
a
n
t
{\displaystyle \ U_{2}=constant}
As
U
2
{\displaystyle \ U_{2}}
is zero on the walls, it should be zero in the whole fully developed region, i.e.
U
2
(
x
2
)
=
0
{\displaystyle \ U_{2}(x_{2})=0}
Momentum Equation in j-direction
ρ
∂
U
j
∂
t
⏟
=
0
S
t
e
a
d
y
+
ρ
U
i
∂
U
j
∂
x
i
=
−
∂
P
∂
x
j
+
ρ
g
j
+
∂
τ
i
j
∂
x
i
{\displaystyle \underbrace {\rho {\frac {\partial U_{j}}{\partial t}}} _{=0\ Steady}+\rho U_{i}{\frac {\partial U_{j}}{\partial x_{i}}}=-{\frac {\partial P}{\partial x_{j}}}+\rho g_{j}+{\frac {\partial \tau _{ij}}{\partial x_{i}}}}
in
x
1
{\displaystyle x_{1}}
direction ,
g
1
=
0
{\displaystyle g_{1}=0}
ρ
U
i
∂
U
1
∂
x
i
⏟
A
=
−
∂
P
∂
x
1
+
∂
τ
i
1
∂
x
i
⏟
B
{\displaystyle \underbrace {\rho U_{i}{\frac {\partial U_{1}}{\partial x_{i}}}} _{A}=-{\frac {\partial P}{\partial x_{1}}}+\underbrace {\frac {\partial \tau _{i1}}{\partial x_{i}}} _{B}}
Consider term A:
ρ
U
i
∂
U
1
∂
x
i
=
ρ
[
U
1
∂
U
1
∂
x
1
⏟
=
0
F
u
l
l
y
−
d
e
v
e
l
o
p
e
d
+
U
2
⏟
=
0
∂
U
1
∂
x
2
+
U
3
⏟
=
0
f
u
l
l
y
−
d
e
v
e
l
o
p
e
d
2
D
∂
U
1
∂
x
3
⏟
=
0
2
D
]
=
0
{\displaystyle \rho U_{i}{\frac {\partial U_{1}}{\partial x_{i}}}=\rho \left[U_{1}\underbrace {\frac {\partial U_{1}}{\partial x_{1}}} _{=0\ Fully-developed}+\underbrace {U_{2}} _{=0}{\frac {\partial U_{1}}{\partial x_{2}}}+\underbrace {U_{3}} _{=0\ fully-developed\ 2D}\underbrace {\frac {\partial U_{1}}{\partial x_{3}}} _{=0\ 2D}\right]=0}
Consider term B:
∂
τ
i
1
∂
x
i
=
∂
τ
11
∂
x
1
⏟
=
0
f
u
l
l
y
−
d
e
v
.
+
∂
τ
21
∂
x
2
+
∂
τ
31
∂
x
3
⏟
=
0
2
D
=
∂
τ
21
∂
x
2
=
d
τ
21
d
x
2
{\displaystyle {\frac {\partial \tau _{i1}}{\partial x_{i}}}=\underbrace {\frac {\partial \tau _{11}}{\partial x_{1}}} _{=0\ fully-dev.}+{\frac {\partial \tau _{21}}{\partial x_{2}}}+\underbrace {\frac {\partial \tau _{31}}{\partial x_{3}}} _{=0\ 2D}={\frac {\partial \tau _{21}}{\partial x_{2}}}={\frac {d\tau _{21}}{dx_{2}}}}
hence
τ
21
=
τ
21
(
x
2
)
{\displaystyle \tau _{21}=\tau _{21}(x_{2})}
.
Thus the momentum equation in
x
1
{\displaystyle x_{1}}
direction reads:
0
=
−
∂
P
∂
x
1
+
d
τ
21
d
x
2
{\displaystyle 0=-{\frac {\partial P}{\partial x_{1}}}+{\frac {d\tau _{21}}{dx_{2}}}}
This equation should be valid for all
x
1
{\displaystyle x_{1}}
and
x
2
{\displaystyle x_{2}}
. This requires that
∂
P
∂
x
1
=
d
τ
21
d
x
2
{\displaystyle {\frac {\partial P}{\partial x_{1}}}={\frac {d\tau _{21}}{dx_{2}}}}
= constant.
Remember
τ
21
{\displaystyle \tau _{21}}
is the stress in
x
1
{\displaystyle x_{1}}
direction on a face normal to
x
2
{\displaystyle x_{2}}
direction.
τ
i
j
=
μ
(
∂
U
i
∂
x
j
+
∂
U
j
∂
x
i
)
−
2
3
δ
i
j
μ
∂
U
k
∂
x
k
{\displaystyle \tau _{ij}=\mu \left({\frac {\partial U_{i}}{\partial x_{j}}}+{\frac {\partial U_{j}}{\partial x_{i}}}\right)-{\frac {2}{3}}\delta _{ij}\mu {\frac {\partial U_{k}}{\partial x_{k}}}}
thus,
τ
21
=
μ
(
∂
U
2
∂
x
1
⏟
=
0
+
∂
U
1
∂
x
2
)
+
0
{\displaystyle \tau _{21}=\mu \left(\underbrace {\frac {\partial U_{2}}{\partial x_{1}}} _{=0}+{\frac {\partial U_{1}}{\partial x_{2}}}\right)+0}
τ
21
=
μ
∂
U
1
∂
x
2
since,
U
1
=
U
1
(
x
2
)
τ
21
=
μ
d
U
1
d
x
2
{\displaystyle \tau _{21}=\mu {\frac {\partial U_{1}}{\partial x_{2}}}\ {\text{since,}}\ U_{1}=U_{1}(x_{2})\ \tau _{21}=\mu {\frac {dU_{1}}{dx_{2}}}}
Thus the momentum equation reads:
∂
P
∂
x
1
=
μ
d
2
U
1
d
x
2
2
{\displaystyle {\frac {\partial P}{\partial x_{1}}}=\mu {\frac {d^{2}U_{1}}{dx_{2}^{2}}}}
This equation can be obtained also by using the Reynold's transport equations for a differential volume.
Treatment of channel flow with the RTT approach
The momentum equation in
x
1
{\displaystyle x_{1}}
direction,
F
S
1
+
F
B
1
⏟
=
0
=
∂
∂
t
∫
C
V
ρ
U
1
d
V
⏟
=
0
+
∫
C
S
U
1
ρ
U
i
n
i
d
A
⏟
=
0
f
u
l
l
y
−
d
e
v
.
{\displaystyle F_{S1}+\underbrace {F_{B1}} _{=0}={\frac {\partial }{\partial t}}\underbrace {\int _{CV}\rho U_{1}dV} _{=0}+\underbrace {\int _{CS}U_{1}\rho U_{i}n_{i}dA} _{=0\ fully-dev.}}
The flux term becomes zero since for fully-developed flow incoming flux is equal to the outgoing flux. Thus,
F
S
1
=
0
{\displaystyle \displaystyle F_{S1}=0}
That is:
(
p
−
∂
P
∂
x
1
d
x
1
2
)
d
x
2
d
x
3
−
(
p
+
∂
P
∂
x
1
d
x
1
2
)
d
x
2
d
x
3
{\displaystyle \left(p-{\frac {\partial P}{\partial x_{1}}}{\frac {dx_{1}}{2}}\right)dx_{2}dx_{3}-\left(p+{\frac {\partial P}{\partial x_{1}}}{\frac {dx_{1}}{2}}\right)dx_{2}dx_{3}}
+
(
τ
21
+
d
x
2
2
∂
τ
21
∂
x
2
)
d
x
1
d
x
3
−
(
τ
21
−
d
x
2
2
∂
τ
21
∂
x
2
)
d
x
1
d
x
3
=
0
{\displaystyle +\left(\tau _{21}+{\frac {dx_{2}}{2}}{\frac {\partial \tau _{21}}{\partial x_{2}}}\right)dx_{1}dx_{3}-\left(\tau _{21}-{\frac {dx_{2}}{2}}{\frac {\partial \tau _{21}}{\partial x_{2}}}\right)dx_{1}dx_{3}=0}
−
∂
P
∂
x
1
d
V
+
∂
τ
21
∂
x
2
d
V
=
0
{\displaystyle -{\frac {\partial P}{\partial x_{1}}}dV+{\frac {\partial \tau _{21}}{\partial x_{2}}}dV=0}
−
∂
P
∂
x
1
+
∂
τ
21
∂
x
2
=
0
{\displaystyle -{\frac {\partial P}{\partial x_{1}}}+{\frac {\partial \tau _{21}}{\partial x_{2}}}=0}
Finally, the governing equation of this kind of flow becomes:
∂
P
∂
x
1
=
μ
d
2
U
1
d
x
2
2
{\displaystyle {\frac {\partial P}{\partial x_{1}}}=\mu {\frac {d^{2}U_{1}}{dx_{2}^{2}}}}
with the following boundary conditions:
x
2
=
0
→
U
1
=
0
{\displaystyle x_{2}=0\rightarrow U_{1}=0}
and
x
2
=
D
→
U
1
=
0
{\displaystyle x_{2}=D\rightarrow U_{1}=0}
Integrating the equation once results in a linear function of
x
2
{\displaystyle x_{2}}
:
μ
d
U
1
d
x
2
=
(
∂
P
∂
x
1
)
x
2
+
c
1
→
τ
21
=
(
∂
P
∂
x
1
)
x
2
+
c
1
{\displaystyle \mu {\frac {dU_{1}}{dx_{2}}}=\left({\frac {\partial P}{\partial x_{1}}}\right)x_{2}+c_{1}\rightarrow \tau _{21}=\left({\frac {\partial P}{\partial x_{1}}}\right)x_{2}+c_{1}}
The second integration reads:
U
1
=
1
2
μ
(
∂
P
∂
x
1
)
x
2
2
+
1
μ
c
1
x
2
+
c
2
{\displaystyle U_{1}={\frac {1}{2\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)x_{2}^{2}+{\frac {1}{\mu }}c_{1}x_{2}+c_{2}}
The integration constants is obtained by using the boundary conditions:
x
2
=
0
,
U
1
=
0
→
c
2
=
0
{\displaystyle x_{2}=0,\ U_{1}=0\rightarrow c_{2}=0}
x
2
=
D
,
U
1
=
0
→
c
1
=
−
1
2
(
∂
P
∂
x
1
)
D
{\displaystyle x_{2}=D,\ U_{1}=0\rightarrow c_{1}=-{\frac {1}{2}}\left({\frac {\partial P}{\partial x_{1}}}\right)D}
Finally, the velocity profile reads:
U
1
=
1
2
μ
(
∂
P
∂
x
1
x
2
2
)
−
1
2
μ
(
∂
P
∂
x
1
)
D
x
2
=
D
2
2
μ
(
∂
P
∂
x
1
)
[
(
x
2
D
)
2
−
(
x
2
D
)
]
{\displaystyle {\begin{array}{lll}U_{1}&=&{\frac {1}{2\mu }}\left({\frac {\partial P}{\partial x_{1}}}x_{2}^{2}\right)-{\frac {1}{2\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)D{x_{2}}\\&=&{\frac {D^{2}}{2\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)\left[\left({\frac {x_{2}}{D}}\right)^{2}-\left({\frac {x_{2}}{D}}\right)\right]\end{array}}}
Note that the velocity profile is parabolic!
The shear stress becomes:
τ
21
=
(
∂
P
∂
x
1
)
x
2
−
1
2
(
∂
P
∂
x
1
)
D
=
D
(
∂
P
∂
x
1
)
[
x
2
D
−
1
2
]
{\displaystyle {\begin{array}{lll}\tau _{21}&=&\left({\frac {\partial P}{\partial x_{1}}}\right)x_{2}-{\frac {1}{2}}\left({\frac {\partial P}{\partial x_{1}}}\right)D\\&=&D\left({\frac {\partial P}{\partial x_{1}}}\right)\left[{\frac {x_{2}}{D}}-{\frac {1}{2}}\right]\end{array}}}
at the wall i.e. at
x
2
{\displaystyle x_{2}}
= 0 and
x
2
{\displaystyle x_{2}}
= D
τ
21
(
0
)
=
−
1
2
D
(
∂
P
∂
x
1
)
{\displaystyle \tau _{21}(0)=-{\frac {1}{2}}D\left({\frac {\partial P}{\partial x_{1}}}\right)}
τ
21
(
D
)
=
1
2
D
(
∂
P
∂
x
1
)
{\displaystyle \tau _{21}(D)={\frac {1}{2}}D\left({\frac {\partial P}{\partial x_{1}}}\right)}
Velocity and shear stress vectors in fully developed channel flow
Note that
τ
21
{\displaystyle \tau _{21}}
is maximum near the wall, i.e. momentum loss is maximum near the wall. This is due to the maximum velocity gradient
∂
U
1
∂
x
2
{\displaystyle {\frac {\partial U_{1}}{\partial x_{2}}}}
near the wall!
The volume flow rate is,
Q
=
∫
A
U
i
n
i
d
A
=
∫
0
D
U
1
w
d
x
2
{\displaystyle Q=\int _{A}U_{i}n_{i}dA=\int _{0}^{D}U_{1}wdx_{2}}
where
w
{\displaystyle w}
is the depth of the channel.
Thus the volume flow rate per depth
w
{\displaystyle w}
is given by:
Q
w
=
∫
0
D
1
2
μ
(
∂
P
∂
x
1
)
(
x
2
−
D
x
2
)
d
x
2
{\displaystyle {\frac {Q}{w}}=\int _{0}^{D}{\frac {1}{2\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)\left(x^{2}-D{x_{2}}\right)dx_{2}}
Q
w
=
−
1
12
μ
(
∂
P
∂
x
1
)
D
3
{\displaystyle {\frac {Q}{w}}=-{\frac {1}{12\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)D^{3}}
Note that
∂
P
∂
x
1
{\displaystyle {\frac {\partial P}{\partial x_{1}}}}
should be constant for the fully developed flow. Hence, for a channel with a finite length
L
{\displaystyle L}
:
∂
P
∂
x
1
=
p
2
−
p
1
L
=
−
Δ
P
L
{\displaystyle {\frac {\partial P}{\partial x_{1}}}={\frac {p_{2}-p_{1}}{L}}={\frac {-\Delta P}{L}}}
Where
Δ
P
{\displaystyle \Delta P}
is the pressure drop along L.
Q
w
=
−
1
12
μ
(
−
Δ
P
L
)
D
3
=
D
3
12
μ
L
Δ
P
{\displaystyle {\frac {Q}{w}}=-{\frac {1}{12\mu }}\left({\frac {-\Delta P}{L}}\right)D^{3}={\frac {D^{3}}{12\mu L}}\Delta P}
or the pressure drop can be calculated from:
Δ
P
=
Q
w
12
μ
L
D
3
{\displaystyle \Delta P={\frac {Q}{w}}{\frac {12\mu L}{D^{3}}}}
For the same flow rate, increasing the height of the channel would cause a drastic reduction in the pressure drop.
The average velocity
U
¯
{\displaystyle {\bar {U}}}
is:
U
¯
=
U
0
=
Q
A
=
Q
w
D
=
−
1
12
μ
(
∂
P
∂
x
1
)
D
3
w
w
D
=
−
1
12
μ
(
∂
P
∂
x
1
)
D
2
{\displaystyle {\bar {U}}=U_{0}={\frac {Q}{A}}={\frac {Q}{wD}}=-{\frac {1}{12\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right){\frac {D^{3}w}{wD}}=-{\frac {1}{12\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)D^{2}}
The maximum velocity occurs when:
d
U
1
d
x
2
=
0
=
D
2
2
μ
(
∂
P
∂
x
1
)
(
2
x
2
D
2
−
1
D
)
{\displaystyle {\frac {dU_{1}}{dx_{2}}}=0={\frac {D^{2}}{2\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)\left({\frac {2x_{2}}{D^{2}}}-{\frac {1}{D}}\right)}
Hence, at
x
2
=
D
2
{\displaystyle x_{2}={\frac {D}{2}}}
,
U
1
=
U
1
m
a
x
{\displaystyle U_{1}=U_{1max}}
U
1
(
D
2
)
=
U
1
m
a
x
=
−
1
8
μ
(
∂
P
∂
x
1
)
D
2
=
3
2
U
¯
{\displaystyle U_{1}\left({\frac {D}{2}}\right)=U_{1max}=-{\frac {1}{8\mu }}\left({\frac {\partial P}{\partial x_{1}}}\right)D^{2}={\frac {3}{2}}{\bar {U}}}
The velocity profile can be written as functions of bulk velocity
U
¯
{\displaystyle {\overline {U}}}
or maximum velocity
U
1
m
a
x
{\displaystyle U_{1max}}
by replacing their value the velocity profile equation:
U
1
=
−
4
U
1
m
a
x
[
(
x
2
D
)
2
−
(
x
2
D
)
]
=
−
6
U
¯
[
(
x
2
D
)
2
−
(
x
2
D
)
]
{\displaystyle {\begin{array}{lll}U_{1}&=&-4U_{1max}\left[\left({\frac {x_{2}}{D}}\right)^{2}-\left({\frac {x_{2}}{D}}\right)\right]\\&=&-6{\overline {U}}\left[\left({\frac {x_{2}}{D}}\right)^{2}-\left({\frac {x_{2}}{D}}\right)\right]\end{array}}}
Same problem can be solved by using moving plates.
Flow through the gap between a cylindrical piston and the surrounding wall
Consider the hydraulic control valve comprising a piston, fitted to a cylinder with a mean radial clearance of 0,005mm. Determine the leakage flow rate. The fluid is SAE low oil (
ρ
{\displaystyle \rho }
= 932
k
g
m
3
{\displaystyle {\frac {kg}{m^{3}}}}
,
μ
{\displaystyle \mu }
=0.018
k
g
m
s
e
c
{\displaystyle {\frac {kg}{m\ sec}}}
at 55ºC). The flow can be assumed to be laminar, steady, incompressible, fully-developed flow.
(
L
a
=
3000
)
{\displaystyle \left({\frac {L}{a}}=3000\right)}
Since
D
a
=
25
0
,
005
{\displaystyle {\frac {D}{a}}={\frac {25}{0,005}}}
= 5000 the flow in the clearance can be accepted to be 2-D, with the depth
w
=
π
⋅
D
{\displaystyle w=\pi \cdot D}
, thus:
Q
w
=
a
3
Δ
P
12
μ
L
{\displaystyle {\frac {Q}{w}}={\frac {a^{3}\Delta P}{12\mu L}}}
Q
=
a
3
Δ
P
12
μ
L
π
D
=
(
0.005
⋅
10
−
3
)
3
12
∗
(
0.018
)
∗
15
⋅
10
−
3
∗
(
20
−
1
)
⋅
10
6
∗
π
∗
25
⋅
10
−
3
{\displaystyle Q={\frac {a^{3}\Delta P}{12\mu L}}\pi D={\frac {(0.005\cdot 10^{-3})^{3}}{12*(0.018)*15\cdot 10^{-3}}}*(20-1)\cdot 10^{6}*\pi *25\cdot 10^{-3}}
Q
=
57.6
⋅
10
−
9
m
3
s
=
57.6
m
m
3
s
e
c
{\displaystyle Q=57.6\cdot 10^{-9}{\frac {m^{3}}{s}}=57.6{\frac {mm^{3}}{sec}}}
Check the Reynolds number to ensure that laminar flow assumption is correct.
U
¯
=
Q
A
=
Q
π
D
a
=
0.147
m
s
e
c
{\displaystyle {\bar {U}}={\frac {Q}{A}}={\frac {Q}{\pi D\ a}}=0.147{\frac {m}{sec}}}
R
e
=
ρ
U
¯
a
μ
=
932
∗
0.147
∗
0.005
⋅
10
−
3
0.018
=
0.0375
{\displaystyle Re={\frac {\rho {\bar {U}}a}{\mu }}={\frac {932*0.147*0.005\cdot 10^{-3}}{0.018}}=0.0375}
Re
<<
1800
{\displaystyle <<1800}
, i. e. the flow is laminar.
This channel flow contains two different and non miscible fluids. Fluids A and B flow at the same time through a channel, which is bounded two flat plates. They both occupy the half height of the channel. The fluid A has a viscosity
μ
A
{\displaystyle \displaystyle \mu _{A}}
, a density
ρ
A
{\displaystyle \displaystyle \rho _{A}}
and the mass flow
m
˙
A
{\displaystyle \displaystyle {\dot {m}}_{A}}
. Fluid B, which is located above fluid A, has a viscosity
μ
B
{\displaystyle \displaystyle \mu _{B}}
, a density
ρ
B
{\displaystyle \displaystyle \rho _{B}}
and the mass flow
m
˙
B
{\displaystyle \displaystyle {\dot {m}}_{B}}
. The following differential equations correspond to the molecular momentum
τ
21
{\displaystyle \displaystyle \tau _{21}}
for each Fluid.
d
τ
21
A
d
x
2
=
d
P
d
x
1
{\displaystyle {\frac {d\tau _{21}^{A}}{dx_{2}}}={\frac {dP}{dx_{1}}}}
and
d
τ
21
B
d
x
2
=
d
P
d
x
1
{\displaystyle {\frac {d\tau _{21}^{B}}{dx_{2}}}={\frac {dP}{dx_{1}}}}
.
With
τ
21
=
μ
d
U
1
d
x
2
{\displaystyle \tau _{21}=\mu {\frac {dU_{1}}{dx_{2}}}}
yields the velocity field:
d
2
U
1
A
d
x
2
=
1
μ
A
d
P
d
x
1
{\displaystyle {\frac {d^{2}U_{1}^{A}}{dx_{2}}}={\frac {1}{\mu _{A}}}{\frac {dP}{dx_{1}}}}
and
d
2
U
1
B
d
x
2
=
1
μ
B
d
P
d
x
1
{\displaystyle {\frac {d^{2}U_{1}^{B}}{dx_{2}}}={\frac {1}{\mu _{B}}}{\frac {dP}{dx_{1}}}}
After integration of both equations we obtain:
τ
21
A
=
d
P
d
x
1
x
2
+
C
1
A
{\displaystyle \tau _{21}^{A}={\frac {dP}{dx_{1}}}x_{2}+C_{1}^{A}}
and
τ
21
B
=
d
P
d
x
1
x
2
+
C
1
B
{\displaystyle \tau _{21}^{B}={\frac {dP}{dx_{1}}}x_{2}+C_{1}^{B}}
As boundary condition we consider that shear stress on the interface between A and B is the same. Therefore we obtain:
τ
21
A
(
x
2
=
0
)
=
τ
21
B
(
x
2
=
0
)
{\displaystyle \tau _{21}^{A}(x_{2}=0)=\tau _{21}^{B}(x_{2}=0)}
Then,
C
1
A
=
C
1
B
=
C
1
{\displaystyle C_{1}^{A}=C_{1}^{B}=C_{1}}
After the integration for the velocity field:
U
1
A
=
1
2
μ
A
d
P
d
x
1
x
2
2
+
C
1
μ
A
x
2
+
C
2
A
{\displaystyle U_{1}^{A}={\frac {1}{2\mu _{A}}}{\frac {dP}{dx_{1}}}x_{2}^{2}+{\frac {C_{1}}{\mu _{A}}}x_{2}+C_{2}^{A}}
and
U
1
B
=
1
2
μ
B
d
P
d
x
1
x
2
2
+
C
1
μ
B
x
2
+
C
2
B
{\displaystyle U_{1}^{B}={\frac {1}{2\mu _{B}}}{\frac {dP}{dx_{1}}}x_{2}^{2}+{\frac {C_{1}}{\mu _{B}}}x_{2}+C_{2}^{B}}
The second boundary condition turns out to be on the interface:
U
1
A
(
x
2
=
0
)
=
U
1
B
(
x
2
=
0
)
{\displaystyle U_{1}^{A}(x_{2}=0)=U_{1}^{B}(x_{2}=0)}
, therefore,
C
2
A
=
C
2
B
=
C
2
{\displaystyle C_{2}^{A}=C_{2}^{B}=C_{2}}
. The integration constants can be calculated with the following boundary conditions:
At
x
2
=
−
D
→
U
1
A
=
0
{\displaystyle x_{2}=-D\ \rightarrow \ \ U_{1}^{A}=0}
:
0
=
d
P
d
x
1
1
2
μ
A
D
2
−
C
1
D
μ
A
+
C
2
{\displaystyle 0={\frac {dP}{dx_{1}}}{\frac {1}{2\mu _{A}}}D^{2}-{\frac {C_{1}D}{\mu _{A}}}+C_{2}}
At
x
2
=
+
D
→
U
1
B
=
0
{\displaystyle x_{2}=+D\ \rightarrow \ \ U_{1}^{B}=0}
:
0
=
d
P
d
x
1
1
2
μ
B
D
2
+
C
1
D
μ
B
+
C
2
{\displaystyle 0={\frac {dP}{dx_{1}}}{\frac {1}{2\mu _{B}}}D^{2}+{\frac {C_{1}D}{\mu _{B}}}+C_{2}}
Therefore we obtain for the velocity distribution in the fluids A and B:
U
1
A
=
−
D
2
2
μ
A
d
P
d
x
1
[
+
2
μ
A
(
μ
A
+
μ
B
)
+
(
μ
A
−
μ
B
μ
A
+
μ
B
)
(
x
2
D
)
−
(
x
2
D
)
2
]
{\displaystyle U_{1}^{A}=-{\frac {D^{2}}{2\mu _{A}}}{\frac {dP}{dx_{1}}}\left[+{\frac {2\mu _{A}}{(\mu _{A}+\mu _{B})}}+\left({\frac {\mu _{A}-\mu _{B}}{\mu _{A}+\mu _{B}}}\right)\left({\frac {x_{2}}{D}}\right)-\left({\frac {x_{2}}{D}}\right)^{2}\right]\ \ \ \ \ }
and
U
1
B
=
−
D
2
2
μ
B
d
P
d
x
1
[
+
2
μ
B
(
μ
A
+
μ
B
)
+
(
μ
A
−
μ
B
μ
A
+
μ
B
)
(
x
2
D
)
−
(
x
2
D
)
2
]
{\displaystyle U_{1}^{B}=-{\frac {D^{2}}{2\mu _{B}}}{\frac {dP}{dx_{1}}}\left[+{\frac {2\mu _{B}}{(\mu _{A}+\mu _{B})}}+\left({\frac {\mu _{A}-\mu _{B}}{\mu _{A}+\mu _{B}}}\right)\left({\frac {x_{2}}{D}}\right)-\left({\frac {x_{2}}{D}}\right)^{2}\right]}
For the distribution of the shear stress we get:
τ
21
=
D
d
P
d
x
1
[
(
x
2
D
)
−
1
2
(
μ
A
−
μ
B
μ
A
+
μ
B
)
]
{\displaystyle \tau _{21}=D{\frac {dP}{dx_{1}}}\left[\left({\frac {x_{2}}{D}}\right)-{\frac {1}{2}}\left({\frac {\mu _{A}-\mu _{B}}{\mu _{A}+\mu _{B}}}\right)\right]}
If we choose
μ
A
=
μ
B
{\displaystyle \displaystyle \mu _{A}=\mu _{B}}
,
U
1
=
−
D
2
2
μ
A
d
P
d
x
1
[
1
−
(
x
2
D
)
2
]
{\displaystyle U_{1}={\frac {-D^{2}}{2\mu _{A}}}{\frac {dP}{dx_{1}}}\left[1-\left({\frac {x_{2}}{D}}\right)^{2}\right]}
τ
21
=
D
d
P
d
x
1
(
x
2
D
)
{\displaystyle \tau _{21}=D{\frac {dP}{dx_{1}}}\left({\frac {x_{2}}{D}}\right)}
The solution gives that of the channel flow. In other words, velocity has a parabolic profile with the peak in the middle of the channel and a linear shear stress distribution
τ
21
{\displaystyle \displaystyle \tau _{21}}
, where
τ
21
=
0
{\displaystyle \displaystyle \tau _{21}=0}
at the channel's centerline.
If
μ
A
≠
μ
B
{\displaystyle \mu _{A}\neq \mu _{B}}
, the position where the maximal velocity occurs can be calculated by introducing
τ
21
=
0
{\displaystyle \displaystyle \tau _{21}=0}
on the velocity profile equation:
x
2
(
U
1
m
a
x
)
=
D
2
(
μ
A
−
μ
B
μ
A
+
μ
B
)
{\displaystyle x_{2}(U_{1max})={\frac {D}{2}}\left({\frac {\mu _{A}-\mu _{B}}{\mu _{A}+\mu _{B}}}\right)}
The shear stress on the upper plate is:
τ
W
B
=
D
2
d
P
d
x
1
[
μ
A
+
3
μ
B
μ
A
+
μ
B
]
{\displaystyle \tau _{W}^{B}={\frac {D}{2}}{\frac {dP}{dx_{1}}}\left[{\frac {\mu _{A}+3\mu _{B}}{\mu _{A}+\mu _{B}}}\right]}
and the shear stress on the lower plate reads:
τ
W
A
=
−
D
2
d
P
d
x
1
[
3
μ
A
+
μ
B
μ
A
+
μ
B
]
{\displaystyle \tau _{W}^{A}=-{\frac {D}{2}}{\frac {dP}{dx_{1}}}\left[{\frac {3\mu _{A}+\mu _{B}}{\mu _{A}+\mu _{B}}}\right]}
The average velocities of the fluids A and B are:
U
~
1
A
=
−
D
2
12
μ
A
d
P
d
x
1
(
7
μ
A
+
μ
B
μ
A
+
μ
B
)
{\displaystyle {\tilde {U}}_{1}^{A}=-{\frac {D^{2}}{12\mu _{A}}}{\frac {dP}{dx_{1}}}\left({\frac {7\mu _{A}+\mu _{B}}{\mu _{A}+\mu _{B}}}\right)}
and
U
~
1
B
=
−
D
2
12
μ
B
d
P
d
x
1
(
μ
A
+
7
μ
B
μ
A
+
μ
B
)
{\displaystyle {\tilde {U}}_{1}^{B}=-{\frac {D^{2}}{12\mu _{B}}}{\frac {dP}{dx_{1}}}\left({\frac {\mu _{A}+7\mu _{B}}{\mu _{A}+\mu _{B}}}\right)}
Hence the respectively mass flow rates are:
m
˙
A
=
B
D
U
~
1
A
{\displaystyle {\dot {m}}_{A}=BD{\tilde {U}}_{1}^{A}}
and
m
˙
B
=
B
D
U
~
1
B
{\displaystyle {\dot {m}}_{B}=BD{\tilde {U}}_{1}^{B}}
Cylindrical coordinates
A change of variables on the Cartesian equations will yield[ 5] the following equations of momentum in r ,
θ
{\displaystyle \theta }
, and x directions for incompressible and isothermal flows (constant density and viscosity):
r
:
ρ
(
∂
u
r
∂
t
+
u
r
∂
u
r
∂
r
+
u
θ
r
∂
u
r
∂
θ
+
u
x
∂
u
r
∂
x
−
u
θ
2
r
)
=
−
∂
p
∂
r
+
μ
[
1
r
∂
∂
r
(
r
∂
u
r
∂
r
)
+
1
r
2
∂
2
u
r
∂
θ
2
+
∂
2
u
r
∂
x
2
−
u
r
r
2
−
2
r
2
∂
u
θ
∂
θ
]
+
ρ
g
r
{\displaystyle r:\;\;\rho \left({\frac {\partial u_{r}}{\partial t}}+u_{r}{\frac {\partial u_{r}}{\partial r}}+{\frac {u_{\theta }}{r}}{\frac {\partial u_{r}}{\partial \theta }}+u_{x}{\frac {\partial u_{r}}{\partial x}}-{\frac {u_{\theta }^{2}}{r}}\right)=-{\frac {\partial p}{\partial r}}+\mu \left[{\frac {1}{r}}{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{r}}{\partial r}}\right)+{\frac {1}{r^{2}}}{\frac {\partial ^{2}u_{r}}{\partial \theta ^{2}}}+{\frac {\partial ^{2}u_{r}}{\partial x^{2}}}-{\frac {u_{r}}{r^{2}}}-{\frac {2}{r^{2}}}{\frac {\partial u_{\theta }}{\partial \theta }}\right]+\rho g_{r}}
θ
:
ρ
(
∂
u
θ
∂
t
+
u
r
∂
u
θ
∂
r
+
u
θ
r
∂
u
θ
∂
θ
+
u
x
∂
u
θ
∂
x
+
u
r
u
θ
r
)
=
−
1
r
∂
p
∂
θ
+
μ
[
1
r
∂
∂
r
(
r
∂
u
θ
∂
r
)
+
1
r
2
∂
2
u
θ
∂
θ
2
+
∂
2
u
θ
∂
x
2
+
2
r
2
∂
u
r
∂
θ
−
u
θ
r
2
]
+
ρ
g
θ
{\displaystyle \theta :\;\;\rho \left({\frac {\partial u_{\theta }}{\partial t}}+u_{r}{\frac {\partial u_{\theta }}{\partial r}}+{\frac {u_{\theta }}{r}}{\frac {\partial u_{\theta }}{\partial \theta }}+u_{x}{\frac {\partial u_{\theta }}{\partial x}}+{\frac {u_{r}u_{\theta }}{r}}\right)=-{\frac {1}{r}}{\frac {\partial p}{\partial \theta }}+\mu \left[{\frac {1}{r}}{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{\theta }}{\partial r}}\right)+{\frac {1}{r^{2}}}{\frac {\partial ^{2}u_{\theta }}{\partial \theta ^{2}}}+{\frac {\partial ^{2}u_{\theta }}{\partial x^{2}}}+{\frac {2}{r^{2}}}{\frac {\partial u_{r}}{\partial \theta }}-{\frac {u_{\theta }}{r^{2}}}\right]+\rho g_{\theta }}
x
:
ρ
(
∂
u
x
∂
t
+
u
r
∂
u
x
∂
r
+
u
θ
r
∂
u
x
∂
θ
+
u
x
∂
u
x
∂
x
)
=
−
∂
p
∂
x
+
μ
[
1
r
∂
∂
r
(
r
∂
u
x
∂
r
)
+
1
r
2
∂
2
u
x
∂
θ
2
+
∂
2
u
x
∂
x
2
]
+
ρ
g
x
.
{\displaystyle x:\;\;\rho \left({\frac {\partial u_{x}}{\partial t}}+u_{r}{\frac {\partial u_{x}}{\partial r}}+{\frac {u_{\theta }}{r}}{\frac {\partial u_{x}}{\partial \theta }}+u_{x}{\frac {\partial u_{x}}{\partial x}}\right)=-{\frac {\partial p}{\partial x}}+\mu \left[{\frac {1}{r}}{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{x}}{\partial r}}\right)+{\frac {1}{r^{2}}}{\frac {\partial ^{2}u_{x}}{\partial \theta ^{2}}}+{\frac {\partial ^{2}u_{x}}{\partial x^{2}}}\right]+\rho g_{x}.}
The continuity equation is:
∂
ρ
∂
t
+
1
r
∂
∂
r
(
ρ
r
u
r
)
+
1
r
∂
∂
θ
(
ρ
u
θ
)
+
∂
∂
x
(
ρ
u
x
)
=
0.
{\displaystyle {\frac {\partial \rho }{\partial t}}+{\frac {1}{r}}{\frac {\partial }{\partial r}}\left(\rho ru_{r}\right)+{\frac {1}{r}}{\frac {\partial }{\partial \theta }}\left(\rho u_{\theta }\right)+{\frac {\partial }{\partial x}}\left(\rho u_{x}\right)=0.}
Treatment of pipe flow with the RTT approach(with infinitesimal cylinder)
It is possible to use the same mathematical treatment like before to find and understand the velocity profile for fully developed flow inside a pipe with diameter D and infinite length. To show the flexibility, the same solution for this problem will be approached via 3 different ways.
Applying the RTT to the infinitesimal cylindrical CV along the symmetry axis of horizontal pipe, in which the flow is fully developed, the conservation of mass and the transport side of the conservation of momentum equation drops. Only remaining term governing this kind of flow is the balance of the forces on the CV in
x
{\displaystyle x}
direction.
(
p
−
∂
P
∂
x
d
x
2
)
π
r
2
−
(
p
+
∂
P
∂
x
d
x
2
)
π
r
2
+
τ
r
x
2
π
r
d
x
=
0
{\displaystyle \left(p-{\frac {\partial P}{\partial x}}{\frac {dx}{2}}\right)\pi r^{2}-\left(p+{\frac {\partial P}{\partial x}}{\frac {dx}{2}}\right)\pi r^{2}+\tau _{r_{x}}2\pi rdx=0}
−
∂
P
∂
x
d
x
π
r
2
+
τ
r
x
2
π
r
d
x
=
0
{\displaystyle -{\frac {\partial P}{\partial x}}dx\pi r^{2}+\tau _{r_{x}}2\pi rdx=0}
Hence,
τ
r
x
=
r
2
∂
P
∂
x
{\displaystyle \tau _{r_{x}}={\frac {r}{2}}{\frac {\partial P}{\partial x}}}
which shows that the stress has a negative value and therefore it is in the negative x-direction.
Treatment of pipe flow with the RTT approach(with infinitesimal hollow cylinder)
This time the pressure and viscous force is considered for a concentric hollow cylinder with radius of R and infinitesimally small thickness dr and length dx(as shown in the image besides) along x-direction. Considering pressure term on the cross-section of cylinder
p
2
π
r
d
r
−
(
p
+
∂
P
∂
x
d
x
)
2
π
r
d
r
→
−
(
∂
P
∂
x
)
2
π
r
d
r
d
x
{\displaystyle p2\pi rdr-\left(p+{\frac {\partial P}{\partial x}}{dx}\right)2\pi rdr\rightarrow -\left({\frac {\partial P}{\partial x}}\right)2\pi rdrdx}
considering viscous shear stress on the surface of the cylinder
(
τ
r
x
+
∂
τ
r
x
∂
r
d
r
)
2
π
(
r
+
d
r
)
d
x
−
τ
r
x
2
π
r
d
x
{\displaystyle \left(\tau _{r_{x}}+{\frac {\partial \tau _{r_{x}}}{\partial r}}dr\right)2\pi (r+dr)dx-\tau _{r_{x}}2\pi rdx}
=
τ
r
x
2
π
r
d
x
+
τ
r
x
2
π
d
r
d
x
+
(
∂
τ
r
x
∂
r
)
2
π
r
d
r
d
x
+
(
∂
τ
r
x
∂
r
)
2
π
r
d
r
2
d
x
⏟
d
r
2
≈
0
−
τ
r
x
2
π
r
d
x
{\displaystyle =\tau _{r_{x}}2\pi rdx+\tau _{r_{x}}2\pi drdx+\left({\frac {\partial \tau _{r_{x}}}{\partial r}}\right)2\pi rdrdx+\underbrace {\left({\frac {\partial \tau _{r_{x}}}{\partial r}}\right)2\pi r{dr}^{2}dx} _{{dr}^{2}\approx 0}-\tau _{r_{x}}2\pi rdx}
→
τ
r
x
2
π
d
r
d
x
+
(
∂
τ
r
x
∂
r
)
2
π
r
d
r
d
x
{\displaystyle \rightarrow \tau _{r_{x}}2\pi drdx+\left({\frac {\partial \tau _{r_{x}}}{\partial r}}\right)2\pi rdrdx}
combining both term,we get the balance equation,
−
(
∂
P
∂
x
)
2
π
r
d
r
d
x
+
τ
r
x
2
π
d
r
d
x
+
(
∂
τ
r
x
∂
r
)
2
π
r
d
r
d
x
=
0
{\displaystyle -\left({\frac {\partial P}{\partial x}}\right)2\pi rdrdx+\tau _{r_{x}}2\pi drdx+\left({\frac {\partial \tau _{r_{x}}}{\partial r}}\right)2\pi rdrdx=0}
it could be rewritten as
−
(
∂
P
∂
x
)
2
π
r
d
r
d
x
+
(
τ
r
x
+
r
∂
τ
r
x
∂
r
)
2
π
d
r
d
x
=
0
{\displaystyle -\left({\frac {\partial P}{\partial x}}\right)2\pi rdrdx+(\tau _{r_{x}}+r{\frac {\partial \tau _{r_{x}}}{\partial r}})2\pi drdx=0}
dividing both side with
2
π
d
r
d
x
{\displaystyle 2\pi drdx}
,we get
−
(
∂
P
∂
x
)
r
+
∂
(
r
τ
r
x
)
∂
r
=
0
{\displaystyle -\left({\frac {\partial P}{\partial x}}\right)r+{\frac {\partial (r\tau _{r_{x}})}{\partial r}}=0}
or,
(
∂
P
∂
x
)
r
=
∂
(
r
τ
r
x
)
∂
r
{\displaystyle \left({\frac {\partial P}{\partial x}}\right)r={\frac {\partial (r\tau _{r_{x}})}{\partial r}}}
integrating both side ,
∫
(
∂
P
∂
x
)
r
d
r
=
∫
∂
(
r
τ
r
x
)
∂
r
d
r
{\displaystyle \int \left({\frac {\partial P}{\partial x}}\right)r\,dr=\int {\frac {\partial (r\tau _{r_{x}})}{\partial r}}dr}
or,
(
∂
P
∂
x
)
r
2
2
=
r
τ
r
x
{\displaystyle \left({\frac {\partial P}{\partial x}}\right){\frac {r^{2}}{2}}=r\tau _{r_{x}}}
or,
(
∂
P
∂
x
)
r
2
=
τ
r
x
{\displaystyle \left({\frac {\partial P}{\partial x}}\right){\frac {r}{2}}=\tau _{r_{x}}}
However,in a laminar flow!
μ
d
U
d
r
=
1
2
r
∂
P
∂
x
{\displaystyle \mu {\frac {dU}{dr}}={\frac {1}{2}}r{\frac {\partial P}{\partial x}}}
integrating,
U
=
r
2
4
μ
(
∂
P
∂
x
)
+
c
1
{\displaystyle U={\frac {r^{2}}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)+c_{1}}
The boundary condition is:
U
=
0
a
t
r
=
R
{\displaystyle U=0\ at\ r=R}
Thus
c
1
{\displaystyle c_{1}}
can be calculated from the boundary condition.
c
1
=
−
R
2
4
μ
(
∂
P
∂
x
)
⇒
U
=
1
4
μ
(
∂
P
∂
x
)
(
r
2
−
R
2
)
{\displaystyle c_{1}=-{\frac {R^{2}}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)\Rightarrow U={\frac {1}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)(r^{2}-R^{2})}
or
U
=
−
R
2
4
μ
(
∂
P
∂
x
)
[
1
−
(
r
R
)
2
]
{\displaystyle U=-{\frac {R^{2}}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)\left[1-\left({\frac {r}{R}}\right)^{2}\right]}
x
:
ρ
(
∂
u
x
∂
t
⏟
s
t
e
a
d
y
s
t
a
t
e
+
u
r
∂
u
x
∂
r
⏟
u
r
=
0
+
u
θ
r
∂
u
x
∂
θ
⏟
u
θ
=
0
+
u
x
∂
u
x
∂
x
⏟
∂
u
x
∂
x
=
0
)
=
−
∂
p
∂
x
+
μ
[
1
r
∂
∂
r
(
r
∂
u
x
∂
r
)
+
1
r
2
∂
2
u
x
∂
θ
2
⏟
=
0
+
∂
2
u
x
∂
x
2
⏟
=
0
]
+
ρ
g
x
⏟
g
x
=
0
{\displaystyle x:\rho \left(\underbrace {\frac {\partial u_{x}}{\partial t}} _{steadystate}+\underbrace {u_{r}{\frac {\partial u_{x}}{\partial r}}} _{u_{r}=0}+\underbrace {{\frac {u_{\theta }}{r}}{\frac {\partial u_{x}}{\partial \theta }}} _{u_{\theta }=0}+\underbrace {u_{x}{\frac {\partial u_{x}}{\partial x}}} _{{\frac {\partial u_{x}}{\partial x}}=0}\right)=-{\frac {\partial p}{\partial x}}+\mu \left[{\frac {1}{r}}{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{x}}{\partial r}}\right)+\underbrace {{\frac {1}{r^{2}}}{\frac {\partial ^{2}u_{x}}{\partial \theta ^{2}}}} _{=0}+\underbrace {\frac {\partial ^{2}u_{x}}{\partial x^{2}}} _{=0}\right]+\underbrace {\rho g_{x}} _{g_{x}=0}}
thus,
∂
p
∂
x
=
μ
[
1
r
∂
∂
r
(
r
∂
u
x
∂
r
)
]
{\displaystyle {\frac {\partial p}{\partial x}}=\mu \left[{\frac {1}{r}}{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{x}}{\partial r}}\right)\right]}
or,
∂
p
∂
x
=
μ
r
[
∂
∂
r
(
r
∂
u
x
∂
r
)
]
{\displaystyle {\frac {\partial p}{\partial x}}={\frac {\mu }{r}}\left[{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{x}}{\partial r}}\right)\right]}
or,
(
∂
p
∂
x
)
r
μ
=
[
∂
∂
r
(
r
∂
u
x
∂
r
)
]
{\displaystyle \left({\frac {\partial p}{\partial x}}\right){\frac {r}{\mu }}=\left[{\frac {\partial }{\partial r}}\left(r{\frac {\partial u_{x}}{\partial r}}\right)\right]}
Now, integrating both side with respect to
r
{\displaystyle r}
, we get
∫
(
∂
p
∂
x
)
r
μ
d
r
=
∫
∂
(
r
∂
u
x
∂
r
)
{\displaystyle \int \left({\frac {\partial p}{\partial x}}\right){\frac {r}{\mu }}dr=\int \partial \left(r{\frac {\partial u_{x}}{\partial r}}\right)}
then,
(
∂
p
∂
x
)
r
2
2
μ
+
C
=
(
r
∂
u
x
∂
r
)
{\displaystyle \left({\frac {\partial p}{\partial x}}\right){\frac {r^{2}}{2\mu }}+C=\left(r{\frac {\partial u_{x}}{\partial r}}\right)}
dividing by r in both side , we get then
(
∂
p
∂
x
)
r
2
μ
+
C
r
=
(
∂
u
x
∂
r
)
{\displaystyle \left({\frac {\partial p}{\partial x}}\right){\frac {r}{2\mu }}+{\frac {C}{r}}=\left({\frac {\partial u_{x}}{\partial r}}\right)}
integrating again with respect to
r
{\displaystyle r}
gives ,
(
∂
p
∂
x
)
r
2
4
μ
+
C
ln
r
+
D
=
U
x
(
r
)
{\displaystyle \left({\frac {\partial p}{\partial x}}\right){\frac {r^{2}}{4\mu }}+C\ln r+D=U_{x}(r)}
Consequently, when
r
=
0
{\displaystyle r=0}
then
U
x
=
U
m
a
x
{\displaystyle U_{x}=U_{max}}
and
ln
r
=
∞
{\displaystyle \ln r=\infty }
, as a result C=0.
On the other hand, when
r
=
R
{\displaystyle r=R}
then
U
x
=
0
{\displaystyle U_{x}=0}
, so
(
∂
p
∂
x
)
R
2
4
μ
+
D
=
0
{\displaystyle \left({\frac {\partial p}{\partial x}}\right){\frac {R^{2}}{4\mu }}+D=0}
or,
D
=
−
(
∂
p
∂
x
)
R
2
4
μ
{\displaystyle D=-\left({\frac {\partial p}{\partial x}}\right){\frac {R^{2}}{4\mu }}}
By putting D to the primitive equation, we get,
U
=
−
R
2
4
μ
(
∂
P
∂
x
)
[
1
−
(
r
R
)
2
]
{\displaystyle U=-{\frac {R^{2}}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)\left[1-\left({\frac {r}{R}}\right)^{2}\right]}
Knowing the velocity profile we can evaluate relevant quantities. The shear stress profile will look like:
τ
r
x
=
μ
d
U
d
r
=
r
2
(
∂
P
∂
x
)
{\displaystyle \tau _{r_{x}}=\mu {\frac {dU}{dr}}={\frac {r}{2}}\left({\frac {\partial P}{\partial x}}\right)}
at r = 0
→
τ
r
x
=
0
{\displaystyle \rightarrow \tau _{r_{x}}=0}
at r = R
→
τ
r
x
=
R
2
(
∂
P
∂
x
)
{\displaystyle \rightarrow \tau _{r_{x}}={\frac {R}{2}}\left({\frac {\partial P}{\partial x}}\right)}
Shear stress distribution in the fully developed laminar pipe flow.
The volume flow rate would read
Q
=
∫
A
r
e
a
U
i
n
i
d
A
=
∫
A
r
e
a
U
2
π
r
d
r
{\displaystyle \displaystyle Q=\int _{Area}U_{i}n_{i}dA=\int _{Area}U2\pi rdr}
Q
=
∫
1
4
μ
(
∂
P
∂
x
)
(
r
2
−
R
2
)
2
π
r
d
r
{\displaystyle Q=\int {\frac {1}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)(r^{2}-R^{2})2\pi rdr}
Q
=
−
π
R
4
8
μ
(
∂
P
∂
x
)
{\displaystyle Q=-{\frac {\pi R^{4}}{8\mu }}\left({\frac {\partial P}{\partial x}}\right)}
When we approximate
∂
P
∂
x
=
−
Δ
P
L
{\displaystyle {\frac {\partial P}{\partial x}}=-{\frac {\Delta P}{L}}}
Q
=
−
π
R
4
8
μ
[
−
Δ
P
L
]
=
π
Δ
P
R
4
8
μ
L
=
π
Δ
P
D
4
128
μ
L
{\displaystyle Q=-{\frac {\pi R^{4}}{8\mu }}\left[{\frac {-\Delta P}{L}}\right]={\frac {\pi \Delta PR^{4}}{8\mu L}}={\frac {\pi \Delta PD^{4}}{128\mu L}}}
Δ
P
=
128
μ
L
π
D
4
Q
{\displaystyle \Delta P={\frac {128\mu L}{\pi D^{4}}}Q}
Increase radius to create drastic reduction in the pressure drop.
The mean velocity is:
U
¯
=
Q
A
=
Q
π
R
2
=
−
R
2
8
μ
(
∂
P
∂
x
)
=
−
D
2
32
μ
(
∂
P
∂
x
)
{\displaystyle {\bar {U}}={\frac {Q}{A}}={\frac {Q}{\pi R^{2}}}={\frac {-R^{2}}{8\mu }}\left({\frac {\partial P}{\partial x}}\right)=-{\frac {D^{2}}{32\mu }}\left({\frac {\partial P}{\partial x}}\right)}
The location where maximum velocity occurs can be found be setting:
d
U
d
r
=
0
→
d
U
d
r
=
1
2
μ
(
∂
P
∂
x
)
r
{\displaystyle {\frac {dU}{dr}}=0\rightarrow {\frac {dU}{dr}}={\frac {1}{2\mu }}\left({\frac {\partial P}{\partial x}}\right)r}
at r = 0
→
{\displaystyle \rightarrow }
U =
U
m
a
x
{\displaystyle U_{max}}
.
U
m
a
x
=
U
(
0
)
=
−
R
2
4
μ
(
∂
P
∂
x
)
=
2
U
¯
{\displaystyle U_{max}=U(0)=-{\frac {R^{2}}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)=2{\bar {U}}}
Note that in a channel was
U
m
a
x
=
3
2
U
¯
{\displaystyle U_{max}={\frac {3}{2}}{\bar {U}}}
.
U
{\displaystyle U}
can be written as a function of
U
m
a
x
{\displaystyle U_{max}}
i.e.
U
=
−
R
2
4
μ
(
∂
P
∂
x
)
⏟
U
m
a
x
[
1
−
(
r
R
)
2
]
{\displaystyle U=\underbrace {-{\frac {R^{2}}{4\mu }}\left({\frac {\partial P}{\partial x}}\right)} _{U_{max}}\left[1-\left({\frac {r}{R}}\right)^{2}\right]}
U
U
m
a
x
=
[
1
−
(
r
R
)
2
]
{\displaystyle {\frac {U}{U_{max}}}=\left[1-\left({\frac {r}{R}}\right)^{2}\right]}
Again, the velocity profile becomes parabolic.
↑ Fox, R.W. and McDonald, A.T., “Introduction to Fluid Mechanics”, John Willey and Sons.
↑ M. Nishi. PhD Thesis Friedrich-Alexander-Universität Erlangen-Nürnberg, 2009.
↑ M. Nishi, B. Ünsal, F. Durst, and G. Biswas. J. Fluid Mech., 614:425–446, 2008.
↑ Durst, F., Ray, S., Unsal, B., and Bayoumi, O. A., 2005, “The Development Lengths of Laminar Pipe and Channel Flows,” J. Fluids Eng., 127, pp. 1154– 1160.
↑ Acheson, D.J.: Elementary fluid dynamics, Clarendon Press, 1990.