simulating flow over circular spillways by using different turbulence models-libre
DESCRIPTION
Flow over circular spillways is explained by using different types of turbulence models. This explains clearly what are all methods can be used for particular problems.TRANSCRIPT
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Engineering Applications of Computational Fluid Mechanics Vol. 6, No.1, pp. 100–109 (2012)
Received: 14 May. 2011; Revised: 18 Aug. 2011; Accepted: 6 Oct. 2011
100
SIMULATING FLOW OVER CIRCULAR SPILLWAYS BY USING DIFFERENT TURBULENCE MODELS
H. Rahimzadeh *, R. Maghsoodi **, H. Sarkardeh # and S. Tavakkol †
* Department of Mechanical Engineering, Amirkabir University of Technology, Tehran, Iran E-Mail: [email protected] (Corresponding Author)
** Department of Civil Engineering, Shahrood Branch, Islamic Azad University, Shahrood, Iran # Hydraulic Structures Division, Water Research Institute (WRI), Tehran, Iran
† Department of Civil and Environmental Engineering, Amirkabir University of Technology, Tehran, Iran
ABSTRACT: Fluent software has been used to simulate flow over a circular spillway and results were compared
with experimental data. As the flow over a circular spillway is turbulent and has a free surface, its characteristics are
complex and often difficult to be predicted. This study assesses the performance of some turbulence models to
predict the hydraulic condition of flow over circular spillways. The Volume of Fluid (VOF) method is applied to
obtain the free surface in each case. Such cases include highly swirling flows, stress-driven secondary flows and
flows over circular spillways. Finally it is concluded that the results of RSM, RNG k-, Realizable k-, SST k-ω
turbulence models agree well with experimental data.
Keywords: circular spillway, numerical simulation, fluent, turbulence models, VOF
1. INTRODUCTION
Circular spillways are typically used for
measuring discharges and as a control device in
water systems. A circular spillway is an overflow
structure with a circular crest. In fact, they
provide a unique relationship between the
upstream head and the discharge. The
characteristics of the flow over circular spillways
have been a subject of interest to many
researchers. Vo (1992) experimentally found the
discharge coefficient of circular spillways as a
function of the dimensionless total head of the
approaching flow. Ramamurthy and Vo (1993a)
applied these equations to predict the velocity
distribution over a cylindrical spillway.
Ramamurthy and Vo (1993b) compared results of
their experiments with others. Chanson and
Montes (1997) described experiments of circular
spillways, with eight cylinder sizes, for several
spillway heights and for five types of inflow
conditions including partially-developed inflow,
fully developed inflow, upstream ramp and
upstream hydraulic jump. Heidarpour and
Chamani (2006) developed a method to predict
the velocity distribution based on the potential
flow past a cylindrical spillway. Hargreaves et al.
(2007) described the validation of CFD for
modelling free surface flows past a broad-crested
weir. Castro-Orgazet et al. (2008) presented a
generalized one-dimensional model with the
assumption of critical flow in a curvilinear
domain. Castro-Orgazand and Chanson (2009)
developed the Bernoulli theorem along a
streamline to flow in open channels. Tadayon
(2009) analysed mean characteristics of
curvilinear flows by using Computational Fluid
Dynamics (CFD). Pettersson and Rizzi (2009)
used Fluent Software to compare two different
turbulence models accuracy in computing local
boundary layer properties with wind tunnel
measurements. Bagheri and Heidarpour (2010)
simulated flow over a circular-crested spillway
with an irrotational vortex to determine the
spillway discharge coefficient and velocity values
over the crest. Yazdi et al. (2010) simulated flow
around a spur dike with free-surface flow by
using fully three-dimensional, Reynolds-averaged
Navier–Stokes equation. They also applied the
volume of fluid method with geometric
reconstruction scheme to model the free-surface
flow. Rahimzadeh et al. (2010) also simulated
flow over stepped spillways by using Fluent
software. Unal and Goren (2011) presented a
comparative study based on the 3D computational
simulations of the flow around a circular cylinder.
They used three different two-equation turbulence
models in their simulations.
2. EXPERIMENTAL DATA
Experimental tests used in this numerical study
were conducted in a smooth channel by Vo
(1992). Six fixed-bed tests were conducted in a
flume with La = 1.800 m, R = 0.152 m and w =
1.164 m (Fig. 1). Other parameters are given in
Table 1.
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Engineering Applications of Computational Fluid Mechanics Vol.6, No. 1 (2012)
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Fig. 1 Schematic view of circular spillway.
Table 1 Selected experimental parameters.
(deg) (deg) H1 (m) Q (L/s/m)
Test 1 90 90 0.1237 85.39
Test 2 90 90 0.1762 152.17
Test 3 90 90 0.2093 203.43
Test 4 60 45 0.0796 41.34
Test 5 60 45 0.1185 80.04
Test 6 60 45 0.1482 115.71
3. TURBULENCE MODELS
In this section different turbulence models which
are used in the present research are briefly
described. In Reynolds averaging:
i i iu u u
(1)
where iu and iu are the mean and fluctuating
velocity components, respectively. Substituting
expressions of this form for the flow variables
into the instantaneous continuity and momentum
equations and simplifying (and dropping the
overbar on the mean velocity, u ), we have
0ii
ut x
(2)
i i jj
u u ut x
2
3
ji lij
i j j i l
i jj
uu up
x x x x x
u ux
(3)
where equations 2 and 3 are called Reynolds-
averaged Navier-Stokes (RANS) equation,
i ju u is called Reynolds stresses, and should
be modelled. Hinze (1975) related the Reynolds
stresses to the mean velocity gradients:
2
3
ji ii j t t ij
j i i
uu uu u k
x x x (4)
The Boussinesq hypothesis is used in the k-, and
k- models.
3.1 Standard k- model (Launder and Spalding, 1972)
The effective viscosity is modelled as follows:
2
t
kC (5)
where C is a constant (Table 2), k is the
turbulence kinetic energy, and is the turbulence
dissipation rate. The following equations are the
transport equations for the standard k- model.
ii
k kut x
t
j k j
k b M
k
x x
G G Y
(6)
ii
ut x
2
1 3 2
t
j j
k b
x x
C G C G Ck k
(7)
Standard constants of the k- model are listed in
Table 2, and were used in the model.
3.2 Renormalization-group (RNG) k- model (Yakhot and Orszag, 1986)
Effective viscosity and transport equations for the
RNG k- model are as follows:
2
31.72
1 100
effkd d
(8)
effˆ
ii
k kut x
k eff k b Mj j
kG G Y
x x
(9)
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Table 2 Standard turbulence models constants.
C1 C2 C1 C2 C k
Standard k- 1.44 1.92 - - 0.09 1.0 1.3
RNG k- 1.42 1.68 - - - - -
Realizable k- 1.44 - - 1.9 - 1.0 1.2
Standard k- - - 0.555 0.83 0.09 2 2
ii
ut x
1 3
32 20
2 3
1
1
eff k bj j
C G C Gx x k
CC
k k
(10)
where k and are computed using the
following formula:
0.6321 0.3679
0 0
1.3929 2.3929
1.3929 2.3929
mol
eff
(11)
where 0 1.0
and
0, 4.38, 0.012Sk
Standard constants of RNG k- model are listed
in Table 2, and were used in the model.
3.3 Realizable k- model (Shih et al., 1995)
The effective viscosity is modelled as follows:
2
t
kC (12)
The difference between the realizable k- model
and the standard and RNG k- models is that C
is no longer constant. It is computed from
*
*
0
1,
2 ,
ij ij ij ij
s
ij ij ijk k ij ij ijk k
C U S SkU
A A
where ij is the mean rate-of-rotation tensor
viewed in a rotating reference frame with the
angular velocity k and
1
0
14.04, 6 , cos 6 ,
3sA A W
, ,ij jk ki
ij ij
S S SW S S S
S
1
2
j iij
i j
u uS
x x
Transport equations of the realizable k- model
are as follows:
ji
k kut x
t
i k j
k b M
k
x x
G G Y
(13)
jj
ut x
1
2
2 1 3
t
j j
b
C Sx x
C C C Gkk
(14)
where
1 max 0.43, ,5
kC S
Standard constants of realizable k- model are
listed in Table 2, and were used in the model.
3.4 The standard k- models (Wilcox, 1998)
The effective viscosity and transport equations of
this model are as follows:
*
t
k
(15)
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Engineering Applications of Computational Fluid Mechanics Vol.6, No. 1 (2012)
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where * damps the turbulent viscosity causing a
low-Reynolds-number correction.
ii
k kut x
tk k
j k j
kG Y
x x
(16)
ii
ut x
t
j j
G Yx x
(17)
Standard constants of k- model are listed in
Table 2, and were used in the model.
3.5 Shear-stress transport (SST) k- model (Menter, 1994)
The effective viscosity and transport equations are
modelled in SST k- model, by equations 18, 19
and 20.
2
*
1
1
21max ,
t
ij ij
k
F
(18)
ii
k kut x
tk k
j k j
kG Y
x x
(19)
ii
ut x
t
j j
G Y Dx x
(20)
where
1 ,1 1 ,2
1,
1k
k kF F
1 ,1 1 ,2
1
1F F
,1 ,1 ,2 ,21.176, 2.0, 1.0, 1.168k w k w
ij is the mean rate-of-rotation tensor,
* is
damps the turbulent viscosity causing a low-
Reynolds-number correction and 1F ,
2F are the
blending functions.
In k- and k-models, kG , bG , G , D and
MY (Sarkar and Balakrishnan, 1990) are the
generation of turbulence kinetic energy due to the
mean velocity gradients, the generation of
turbulence kinetic energy due to buoyancy, the
generation of , the cross-diffusion term, and the
contribution of the fluctuating dilatation in
compressible turbulence to the overall dissipation
rate, respectively.
3.6 Reynolds stress model (RSM) (Launder et al., 1975; Gibson and Launder, 1978; Launder, 1989a and b)
The turbulence stress components are,
ij
i j k i jk
Local Time Derivative C Convection
u u u u ut x
,
,
T ij
L ij
i j k kj i ik jk
D Turbulent Diffusion
i jk k
D Molecular Diffusion
u u u p u ux
u ux x
Pr
Prij
ij
j ii k j k i j j i
k kG Buoyancy oduction
P Stress oduction
u uu u u u g u g u
x x
Pr
Pr
2
2
ijij
ij
j ji i
j i k k
Dissipationessure Strain
k j m ikm i m jkm
F oduction by System Rotation
u uu up
x x x x
u u u u
(21)
Of the various terms in the above transport
equation, ijC , ,L ijD , ijP , and ijF do not require
any modeling. However, ,T ijD (Lien and
Leschziner, 1994), ijG , ij (Gibson and Launder,
1978;, Fu et al., 1987;, Launder, 1989a and b),
and ij need to be modeled to close the equations.
To simulate the pressure strain (ij), Linear
pressure-strain is used.
4. FREE SURFACE MODELLING
The volume of fluid (VOF) method appears to be
a powerful computational tool for the analysis of
free-surface flows (Hirt and Nichols, 1981). The
tracking of the interface(s) between the phases is
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Engineering Applications of Computational Fluid Mechanics Vol.6, No. 1 (2012)
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accomplished by the solution of a continuity
equation for the volume fraction of one (or more)
of the phases. For the qth
phase, this equation has
the following form:
. . 0q
qt
(22)
where q is the volume fraction of qth phase. In
each control volume, the volume fractions of all
phases sum up to unity. The following three
conditions are possible for each cell:
0q : the cell is empty (of the qth phase).
1q : the cell is full (of the qth phase).
0 1q : the cell contains the interface
between the qth phase and one or more other
phases.
It can be assumed the free surface is on the
volume fraction of 0.5 (Fluent Manual 2005,
Dargahi 2006). In each cell the average properties
are computed according to the volume fraction of
each phase. For example, density and dynamic
viscosity in each cell of two phases are:
1 1 1 21 , 1 1 1 21 ,
respectively. The phases are represented by the
subscripts 1 and 2.
In this research, the geometric reconstruction
method of Young (1982) is employed. This
method represents the interface between fluids
using a piecewise-linear approach. It assumes that
the interface between two fluids has a linear slope
within each cell, and uses this linear shape for
calculation of the advection of fluid through the
cell faces.
5. BOUNDARY CONDITIONS AND MESH GENERATION
Both structured and unstructured meshes have
been used. Denser mesh was used around the
spillway, close to free surface and in the boundary
layer in order to provide a higher accuracy and
considering the viscous flow. The first grid
surface of the solid boundaries was at
0.0005y , which ensures that the first grid
surface off the wall is located almost everywhere
at *1.0y y u y and that at least two
grid surfaces are located within the laminar sub-
layer (y+< 5.0), where y is the distance of the
first grid from the solid wall, *u is wall shear
stress, and is kinetic viscosity (Fig. 2).
(a)
(b)
(c)
Fig. 2 Computational grid in the vicinity of spillway:
(a) 3D view, (b) horizontal view, (c) near the
crest.
Fig. 3 Solution domain and boundaries for modelled
circular spillway.
Boundary conditions which were employed in this
investigation are (Fig. 3): Two different inlets
were needed to define the water flow (Inlet I) and
air flow (Inlet II). These inlets were defined as
stream-wise velocity inlets that require the values
of velocity. To estimate the effect of walls on the
flow, empirical wall functions known as standard
wall functions (Launder and Spalding, 1974) were
used. The upper boundary above the air phase
was specified as a symmetry condition, which
enforces a zero normal velocity and a zero shear
stress.
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To complete the description of the CFD
simulation, the PRESTO pressure discretization
scheme was applied as it showed the best
convergence in this simulation. The first order
upwind momentum and turbulent kinetic energy
discretization scheme was applied (Karki and
Patankar, 1989). The PISO pressure-velocity
coupling algorithm (Issa, 1986) was used purely
because it is designed specifically for transient
simulations. The unsteady, free-surface
calculations required fine grid spacing and small
initial time steps. The grid spacing used was
adequate for solution convergence and has shown
good agreement with the experimental results. A
time step equal to 0.001 was selected. During the
3D simulation runs, solution convergence and the
water-surface profiles were monitored.
Convergence was reached when the normalized
residual of each variable was in the order of 0.001.
The free surface was defined by a value of VOF =
0.5, which is a common practice for volume
fraction results (Fluent Manual, 2005 and Dargahi,
2006). After the convergence of the numerical
solution, in order to obtain more accurate results,
the mesh was refined according to gradients of
two phases and velocities, and the model was run
subsequently. The final number of mesh in
various conditions changed in the range of
187026–202881 cells. A sensitivity analysis was
used and the number of mesh increased to over
two times, which has shown the results of the
model were valid.
6. VERIFICATION
It was necessary to ensure the accuracy of the
model before employing the numerical model.
For this purpose, experimental cases which were
mentioned in previous sections were employed.
To evaluate the free surface, the first case was
selected regarding the available flume data.
Existing experimental results used for validation
include water surface profiles, pressure
distributions and streamwise velocity distributions
for flow over the circular spillways. Fig. 4
compares experimental results of Tests 1, 2 and 3
(considering Table 1 parameters) with computed
water surface profiles over the crest.
Fig. 4 shows that different turbulence models
have no meaningful effect on predicting the free
surface in this simulation. Therefore all numerical
results are on one line. Results of velocity
simulation were compared with all experimental
tests (Table 1) and have been shown in Fig.5.
This figure shows good agreement between
measured and computed velocities by different
turbulence models except the standard k-, the
standard k-, and the k- RNG models.
Fig. 6 compares the pressure profile at crest,
obtained from simulation and experimental results
in different tests.
Fig. 5 and 6 show that the results from standard
models do not have a good agreement with
experimental data. It could be concluded that in
standard turbulence models (k- and k-), both
models under curvature conditions do not have
good performance in predicting hydraulic
characteristics.
In Fig. 7 and Fig. 8, numerical velocity vector
field and the corresponding flow patterns
represented by the streamlines for the flow
upstream of the spillway are given for two
extreme available cases.
7. CONCLUSIONS
In the present numerical study, flow over circular
spillways was simulated by using a three
dimensional code (Fluent Software). Different
turbulence models with the VOF method for free
surface modelling were employed to simulate
fully 3D flow. The numerical simulation solved
the Navier–Stokes equations within the flow
domain upstream and downstream from a
spillway. In the present research, focus was on
performance of different turbulence models to
simulate the flow over the circular spillways. By
comparing the 3D simulation results with the
flume data obtained by other researchers, the
simulation was found to produce flow over a
circular spillway with sufficient accuracy by all
turbulence models except the standard k- and the
standard k-. The RSM turbulence model had the
best agreement among all turbulence models with
experimental data.
Fig. 4 Water surface profiles for flow over circular
spillway.
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(a) Test 1 (b) Test 2
(c) Test 3 (d) Test 4
(e) Test 5 (f) Test 6
Fig.5 Comparison between computed and measured horizontal velocity profiles at the crest of circular spillway by
employing different turbulence models.
NOMENCLATURE
ui velocity component
iu mean velocity component
iu fluctuating velocity component
*u wall shear stress
jiuu Reynolds stresses
density of fluid
p pressure
µ viscosity of fluid
µt turbulent viscosity
µeff effective viscosity
ij Kronecker delta
k turbulence kinetic energy
turbulence dissipation rate
Gk generation of turbulence kinetic energy
due to the mean velocity gradients
Gb generation of turbulence kinetic energy
due to buoyancy
G generation of turbulence kinetic energy
due to
YM contribution of the fluctuating dilatation
in compressible turbulence to the overall
dissipation rate
Yk dissipation of k due to turbulence
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(a) Test 1 (b) Test 2
(c) Test 3 (d) Test 4
(e) Test 5 (f) Test 6
Fig.6 Comparison between computed and measured pressure head distributions at crest of spillway by employing
different turbulence models.
Y dissipation of due to turbulence k turbulent Prandtl number for k
turbulent Prandtl number for turbulent Prandtl number for
ij the mean rate-of-rotation tensor viewed
in a rotating reference frame with the
angular velocity k
S modulus of the mean rate-of-strain
tensor specific dissipation rate
ij mean rate of rotation tensor
F1& F2 blending functions
α* Parameter used to damp the turbulent
viscosity causing a low-Reynolds-
number correction term
Cij convection term
D cross diffusion term
DT,ij turbulent diffusive transport
DL,ij molecular diffusion
Pij stress production
Gij effects of buoyancy on turbulence ij pressure strain
ij dissipation rate
Fij production by system rotation
αq volume fraction of qth phase
y distance of first grid from solid wall
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Case 1
Case 6
Fig.7 Numerical field velocity vectors.
Case 1
Case 6
Fig.8 Numerical field velocity streamlines.
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