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Influence of a gap on flow
around horizontal cylinder
Zdenek Chara1,
Pavel Vlasak1, Jaroslav Pollert jun. 2
1 Institute of Hydrodynamics, ASCR, Pod Patankou
5, Prague 6, Czech Republic
2 CTU - LERMO, Prague 6, Thakurova 7, Czech
Republic
1 Pod Patankou 5, Prague 6, 166 12, Czech
Republic
Tel.:+420-2-24310671, Fax: +420-2-322181,
E-mail: chara@ih.cas.cz, ih@ih.cas.cz
Abstract
The paper presents results of an experimental
investigation of an open channel flow around horizontal circular cylinder
placed at different positions above smooth bed for cylinder Reynolds numbers in
the range 2.103-104. The main attention was paid to the
detail investigation of velocity distribution along a vertical going through
the center of the cylinder. The experiments were conducted for two flow regimes
- shallow flow (when the cylinder behaves like a weir) and backwater flow (when
the water surface is practically unaffected by the presence of the cylinder).
Based on measured velocity profiles the ratios of mean and maximal velocities
through the gaps to the velocities over the cylinder were determined as well as
the shear velocities on the channel bed. The computational software Fluent was
used to simulate both types of flow over the cylinder and the results were
compared with the experimental results.
Keywords:
LDA measurements, numerical simulation, open channel, flow around cylinder
Introduction
A lot of research work has been carried out in
the field of an open channel flow around horizontal circular cylinder placed
perpendicularly to the flow direction. Such arrangement can simulate many
engineering applications - subaqueous pipelines or cables, flow around elements
consolidating channel beds or flow around natural obstacles (fallen trees in
rivers).
Bearman and Zdravkovitch (1978) investigated
the influence of gap between the cylinder and bed on vortex shedding and
pressure distribution on the bed and on the cylinder. Fredsoe and Hansen (1987)
used a propeller to measure the velocity profiles in the gap and between the
top of the cylinder and water surface. They reported that the gap flow velocity
was nearly equal to the velocity of flow above the cylinder in the contrary to
the potential theory that predicts increase the gap flow velocity when the gap
itself is decreasing. Chiew (1991) measured the velocity distribution over a
horizontal cylinder and pressure distribution around the cylinder placed in the
shallow flow where the high blockage ratio of the cylinder leaded to the
choking of the flow. He presented some
function describing a gap flow rate in the dependency of undisturbed approach
flow depth, gap size and diameter of the cylinder.
The present study is focused on the LDA
measurements of longitudinal velocity distribution in the gap and also in the
part over the cylinder. From the velocities measured near the bed the shear
velocities were estimated in the dependency of the gap opening. Second part of
the paper shows comparison of experimental results with the simulation of the
flow by the commercial software Fluent (V4.4).
Experimental
arrangements
The experiments were performed in a horizontal
laboratory flume 5.6 m long, 0.25 m wide and 0.25 m deep. Both bed and walls
were made from glass tables to ensure hydraulic smooth conditions. To control
the water level downstream end of the channel was equipped by the controlled
weir. Two flow regimes were investigated - normal (shallow) flow and backwater
flow. To justify the shallow flow condition the controlled weir was not used.
The depth was relatively low and the cylinder itself acted as some kind of a
weir and hence upstream the cylinder the depth was always higher than the
original value of undisturbed flow.
In the second case (backwater flow) the
controlled weir increased the water depth, mean velocity decreased and the
cylinder did practically not affect the water surface.
Three Plexiglas cylinders of diameters 12, 20
and 30 mm were used for the backwater flow tests and the same cylinders plus a
cylinder of diameter 6 mm were used for the shallow flow tests.
Reynolds numbers based on diameter of the
cylinder and approaching velocity were in the range 2.103-104.
The cylinders were placed 3.8m downstream the entrance section and fixed
directly on side walls. The undisturbed flow depths h0 (depths of flow without the cylinder measured in the
location where the cylinders were fixed) varied from 0.074 to 0.11 m in the
backwater flow, in the shallow flow the depth h0 was 0.0425 m.
The unit flow rate was kept on constant value q=19.1l/s/m. Main
hydraulic parameters of flows without the cylinder are summarized in Table 1.
Shear velocities were estimated from velocity gradient measured near the
channel bed.
|
flow type |
h0 [m] |
Umo [m/s] |
Re |
Fr |
U*o [m/s] |
|
|
0.11 |
0.174 |
40700 |
0.17 |
0.0089 |
|
backwater |
0.091 |
0.210 |
44300 |
0.22 |
0.0105 |
|
|
0.074 |
0.258 |
48000 |
0.30 |
0.0128 |
|
shallow flow |
0.0425 |
0.449 |
57000 |
0.70 |
0.0235 |
Table 1.
The velocity profiles were measured by the
differential LDA system in the middle of the channel width, where quasi
two-dimensional flow was observed. The system consisted of the argon-ion laser
Coherent Innova 70 and the LDA components (including beam expender) assembled
from the Dantec optical system 55X. The Dantec Burst Spectrum Analyzer (BSA-enhanced)
was used to process velocity data collected in backscatter mode. All optical parts (transmitting section, receiving photomultiplier as well as the
argon-ion laser) were placed on a remote controlled xyz support that enabled precise location of a measuring volume.
Results and discussion
Fig. 1 shows several non-dimensional velocity
profiles in the backwater flow measured in the gap for different cylinder
diameters and different gap openings. The velocities and the vertical
coordinates are non-dimensioned by the average gap velocity and by the height
of the gap, respectively. Similar shapes of the gap velocity profiles were also
observed in the shallow flow.

Fig. 1 Velocity profiles in the gap for backwater flow
Fig. 2 shows the influence of the gap opening
on the ratio of the maximal velocities just below the cylinders to those over
the cylinders in both flow regimes. The gap opening is normalized by critical
gap height Gcrit. The
critical gap height is gap opening for which all flow is going only through the
gap. This value depends on the cylinder diameter and the undisturbed flow depth
h0 and from the
experimental data the following relations were found
(1)
The second relation (for G/D>2.15) is very
close to the equation published by Chiew (1991). As can be seen in the Fig. 2
the ratio of maximal velocities is increasing with decreasing gap height that
is in accordance with potential theory, but the values are much smaller
(0.9-1.1) than values predicted by potential theory.

Fig. 2 Ratio of maximal velocities under and over the cylinder
Since the flow in the gap is accelerating the
streamwise negative pressure gradient (favourable pressure gradient- FPG) is
increasing. The effect of FPG on flow properties may be among other described
by the accelerating parameter K. Due to the circular shape of the obstacle the
parameter K is just zero in the gap under the cylinder, but very close upstream
of the measuring position the parameter K achieved values greater than 3.10-6.
For such high values of parameter K a departure of velocity profile from
standard log-law profile could be expected, Warnack and Fernholz (1998). This
was confirmed by the experiments as can be seen in Fig. 3, where an example of
semi-logarithmic plot of U+ versus y+ is shown for
backwater flows under the cylinder of diameter 12 mm. For comparison, a
theoretical log-law profile according Coleman and Alonso (1983) is attached,
too. This theoretical curve was in very good agreement with our experimental
data measured in the flows without cylinders. The gap velocity data lie partly
above the theoretical log-law profile mainly in the viscous sublayer where
follow linear relation (U+=y+) much longer than for
normal flow.

Fig. 3 Non-dimensional velocity profiles in the backwater flow for cylinder of diameter 12 mm
Based on the measured velocities in the laminar
sublayer the shear velocities on the channel bed in vertical passing through
cylinder axis were estimated supposing that the linear relation (U+=y+)
is satisfied. The influence of gap
openings on shear velocities is shown in Fig. 4. The shear velocities were
normalized by those for flows without cylinders. For gap opening G/D greater than 2 the shear velocities are about
20% higher than for undisturbed flow, for minimal gap sizes (G/D<0.1) the
shear velocities are more than 2 times higher.

Fig. 4 Variation in shear velocities at channel bed with gap opening
Comparison of
calculated and measured velocity profiles
To simulate flow around circular obstacles the
program Fluent (V4.4) was used. Two flow patterns were simulated -the cylinder
of diameter 30 mm was placed on the bed (G=0) both in backwater and shallow
flow. Implemented
model was applied
with time step 0.0002 sec. The results are presented in Fig. 5 and 6. Fig. 5
shows non-dimensional plot of measured and calculated velocity profiles over
the cylinder both in the backwater flow and the shallow flow. The velocities
are normalized by average velocity. The
measured velocities in backwater flow are practically constant but the
calculated values significantly differ mostly near the cylinder surface. In the
case of the shallow flow the measured and calculated data are in better
coincidence. In this case the program predicts smaller velocities near the
cylinder surface. Fig.6 presents measured and calculated shape of water surface
over the cylinder in the case of shallow flow. The calculated curve fits the
experimental data quite good mainly downstream the cylinder. In the upstream
part the calculated water surface is slightly bellow the measured data.

Fig. 5 Comparison of measured and calculated velocity profiles over the cylinder

Fig. 6 Comparison of measured and calculated water surface over the cylinder
Conclusion
From the presented paper several conclusion can
be drawn:
·
According
to the potential theory the ratio of maximal velocities under and over the
cylinder increases with decreases gap opening, but the values vary only in the
range 0.9-1.1.
·
The
velocity profiles in the gap significantly differ from theoretical log-law
profile due to the strong favourable pressure gradient
·
The
simulation program Fluent gives relatively good results for shallow flow, but
for backwater flow it greatly overestimates velocities near the cylinder
surface.
Acknowledgement
This research was supported in part under Grant No. A2060603 of the Grant Agency of the ASCR, Project No. VS988037 of the Ministry of Education and Grant No. 103/97/0860 of the Czech Grant Agency.
NOTATION
D = diameter of cylinder
G = gap size
Gcrit = gap
size for which all flow is going through the gap
K = accelerating parameter (K=n/U2(dU/dx))
h = flow depth
ho = undisturbed flow depth
htop = flow depth above the cylinder
q = unit flow rate
Re =
Reynolds number based on hydraulic radius
Fr =
Froude number
U = longitudinal velocity component
Um = mean
velocity
Umo = undisturbed mean velocity
Um bot = mean velocity in the gap
Utop =
maximal velocity above the cylinder
Ubot =
maximal velocity bellow the cylinder
U* = shear
velocity at bed
U*o =
undisturbed shear velocity at bed
U+ =
normalized
(dimensionless) local longitudinal velocity (U+=U/U*)
x =
streamwise direction
y =
vertical direction with the origin at the channel bed
y+ =
dimensionless y-coordinate (y+= y U* /n)
REFERENCES
[1] Bearman, P.W., and Zdravkouvich, M.M. (1978), J. Fluid. Mech., 89 (1),33-47.
[2] Chiew, Y.M. (1991), J. Wtrway., Port, Coast. and Oc. Engrg., ASCE, 117 (2), 120-135
[3] Coleman, N.L., and Alonso, C.V. (1983), J. Hydr. Engrg., ASCE, 109 (2), 175-188.
[4] Fredsoe, J., and Hansen, E.A. (1987), J. Wtrway., Port, Coast., and Oc. Engrg., ASCE, 113 (2); 139-155.
[5] Warnack, D., and Fernholz, H.H. (1998), J. Fluid Mech., 359, 357-381