st.-petersburg state polytechnic university department of aerodynamics, st.-petersburg, russia
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“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg. Numerical analysis of turbulent Rayleigh-Bénard convection in confined enclosures using a hybrid RANS/LES approach. A. ABRAMOV, N. IVANOV & E. SMIRNOV. St.-Petersburg State Polytechnic University - PowerPoint PPT PresentationTRANSCRIPT
St.-Petersburg State Polytechnic University Department of Aerodynamics, St.-Petersburg, Russia
A. ABRAMOV, N. IVANOV & E. SMIRNOV
Numerical analysis of turbulentRayleigh-Bénard convection in confined enclosures
using a hybrid RANS/LES approach
E-mail: [email protected]
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Introduction
Problem description
Mathematical model
Computational aspects
Structure of turbulent convection
Heat transfer predictions
Conclusions
OUTLINE
Abramov et al. SPTU, Russia
1. Full Direct Numerical Simulation (DNS): no turbulence model
2. Under-resolved (coarse-grid) DNS: no turbulence model
3. Unsteady Reynolds-Averaged Navier-Stokes (RANS): modeling of all-scales background turbulence
4. Large Eddy Simulation (LES): modeling of subgrid-scale turbulence
5. RANS/LES hybridization, in particular, non-standard DES
3D Unsteady formulations: modeling levels
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Problem descriptionHigh-Ra Rayleigh-Bénard mercury and water
convection in confined enclosures
H
z
H
D = H
z
r
g Cold walls, Tc
Hot walls, Th
Adiabaticwalls
Mercury,Pr = 0.025
Water,Pr = 7Ra > 108
THgVb - buoyancy velocity
ch TTT
Scales:
a
3THgRa
aPr
H
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Mathematical model Navier-Stokes equations averaged/filtered for a RANS/LES model; Boussinesq’s approximation for gravity buoyancy
zeff TeDiv*pt
SVVV 2Div
TTtT
eff aV
0 V
,ppp h* where ,RaPr/ teff
tteff Pr/PrRa/ 1a
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Turbulence Modelling:RANS / LES one-equation turbulence model
(Abramov & Smirnov, 2002)
ykRe),(RefF,yCl,Fl
kyy
RANS 432
3
2
3kCLES 3
zyx
klfC tt
C,Flminlt
151 .A,A
ReexpF y
0101 .A,A
Reexpf y
LESRANS.
tjk
t
j
,maxSxk
xdtdk
22
Modified Wolfshtein model for a RANS zone:
750.C
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
3D Navier-Stokes code SINF Features of the last version (June 2003):
steady and unsteady computation options, stationary and rotatingreferences
conjugate heat transfer in solid-liquid subdomains multi-component mass transfer a number of RANS turbulence models implemented LES and RANS/LES possibilities for domains of complex geometry
block-structured matching and non-matching body-fitted grids second-order physical time stepping second-order finite-volume spatial discretization various upwind schemes, implicit solvers, parallel version
Computational aspects
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Computational program
Grids of about 160000 cells
Water convection:Ra = 5108; 5109
Pr = 7
Conditions of experiments:Zocchi et al. (Physica A.,1990)
Cioni et al. (J. Fluid Mech.,1997)Qiu et al. (Phys. Rev. E., 1998) etc.
Mercury convection:108 < Ra < 5109
Pr = 0.025
Conditions of experiments:Takeshita et al. (Phys. Rev. Lett.,1996)
Cioni et al. (J. Fluid Mech.,1997)Glazier et al. (Nature, 1999)
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Structure of turbulent convection
0.5
0.5
0.70.9
0.50.30.2
0.6
0.4
0.7
0.4Vb
Mercury convection:Ra = 108, Pr = 0.025
Vb
Velocity vector patterns
Temperature isolines
Vertical velocity at middle
horizontal planew
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Structure of turbulent convectionMercury convection:Ra = 108, Pr = 0.025
Equiscalar surfaces of vertical velocity
w = 0.25 (gray) andw = -0.25 (black)
Temperature and velocity vector fields
Vertical velocity distributions(time-averaging over the interval
of 10 time units)
w
0 1 0 0 2 0 0 3 0 0-0 .5 0
-0 .2 5
0 .0 0
0 .2 5
0 .5 0W
Abramov et al. SPTU, Russia
Structure of turbulent convection
B
A
A
B
A
B
Velocity vector and temperature fields
Water convection:Ra = 5109, Pr = 7
Equiscalar surfaces of vertical velocity
w = 0.05 (black) andw = -0.05 (gray)
A
B
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Abramov et al. SPTU, Russia
Characteristics of the global circulation
0 .0 0 .2 0 .4 0 .6 0 .80 .0
0 .2
0 .4
0 .6
0 .8
1 .0
108
5108
8.7108
z
Th
0 .0 0 .4 0 .8 1 .20 .0
0 .2
0 .4
0 .6
0 .8
1 .0
108
5108
8.7108
wm
z
wmc=2Vg
0 .0 0 .2 0 .4 0 .60 .0
0 .2
0 .4
0 .6
0 .8
1 .0
5108
5109
z
Th
0 .0 0 .2 0 .4 0 .60 .0
0 .2
0 .4
0 .6
0 .8
1 .0
wm
z
5108
5109
Profiles of maximum horizontal temperature difference and vertical velocity difference
Water Mercury
Reynolds number Reg = VgH /, versus Rayleigh number. Mercury
Abramov et al. SPTU, Russia
Temperature isosurface T = 0.9 colored by vertical velocity
1 0 0 1 5 0 2 0 00 .2
0 .4
0 .6
0 .8
1 .0
Temperature fluctuations near the bottom wall (z = 0.03, r = 0)
Thermal plumes in high-Ra convection
0 5 0 1 0 0 1 5 0 2 0 00 .4 0
0 .4 5
0 .5 0
0 .5 5
Temperature isosurfaces T = 0.45 and T = 0.55
Temperature fluctuations near the top wall (z = 0.96)
TT
Ra = 5109Ra = 5108
w
plumes
plumes
Abramov et al. SPTU, Russia
0 1 0 0 2 0 0 3 0 00 .3
0 .4
0 .5
0 .6
0 .7T
0 .0 1 0 .1 1 f1 E -8
1 E -7
1 E -6
1 E -5
1 E -4
1 E -3
1 E -2
0 .1
1E T -5/3
-4
Mercury, Ra = 5108
z = 0.5
0 1 0 0 2 0 0 3 0 0-0 .5 0
-0 .2 5
0 .0 0
0 .2 5
0 .5 0W
0 .0 1 0 .1 1 f1 E -8
1 E -7
1 E -6
1 E -5
1 E -4
1 E -3
0 .0 1
0 .1
1
1 0E W
-5/3
-4
0 5 0 1 0 0 1 5 0 2 0 00 .4 0
0 .4 5
0 .5 0
0 .5 5
0 4 0 8 0 1 2 0 1 6 0 2 0 0-0 .1 0
-0 .0 5
0 .0 0
0 .0 5
0 .1 0
Turbulent vertical velocityand temperature fluctuations
z = 0.75
T
W
Water, Ra = 5109
z
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Abramov et al. SPTU, Russia
Boundary layers near the isothermal walls
0 .0 0 0 .0 5 0 .1 0 0 .1 50 .0
0 .2
0 .4
0 .6
0 .8
1 .0
5108
5109
z
uh
Thermal and viscous boundary layer thicknesses as functions of Ra
Temperature profile near the top wall (mercury)
Mean horizontal velocity profile (water)
Mercury:V < T
Water:V > T
T
0 .0 0 .2 0 .4 0 .60 .9 0
0 .9 2
0 .9 4
0 .9 6
0 .9 8
1 .0 0
z
T
108
5108
8.7108
1 E + 8 1 E + 9
1 E -3
0 .0 1
0 .1
- RANS/LES in water- RANS/LES in mercury- DNS Verzicco et al., 99- Experiment Takeshita et al., 96
Ra
T
1 E + 8 1 E + 9
1 E -3
0 .0 1
0 .1 - DNS Verzicco et al., 99- Experiment Takeshita et al., 96
- RANS/LES in water- RANS/LES in mercury
Ra
V
Ra
Ra
Abramov et al. SPTU, Russia
Heat transfer predictions
0 1 0 0 2 0 0 3 0 0 4 0 02 0
3 0
4 0
5 0Ra = 5108
t
Nu
0 .0 1 0 .1 11 E -7
1 E -6
1 E -5
1 E -4
1 E -3
0 .0 1
0 .1
1
-5/3
-4
fq
f
Eq
0 1 0 0 2 0 0 3 0 0 4 0 0 5 0 0
8 8
9 2
9 6
1 0 0Nu
Nusselt number fluctuations in mercury and water convection
Ra = 5109
1 E + 8 1 E + 9 1 E + 1 0
1 0
1 0 0
- RANS/LES in water- RANS/LES in mercury- Exp. Cioni et al., 96- Exp. Goldstein, 80- Exp. Glazier, 99
Nu
Ra
t
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg
Abramov et al. SPTU, Russia
Numerical simulations of high-Ra R-B convection was performed with a non-standard DES approach based on the one-equationk-model of unresolved turbulence
The specific patterns of fully developed turbulent convection were analyzed, especially the formation of a large-scale circulation cell and thermal plumes for both the configurations
In mercury the global circulation, velocity and temperature fluctuations are considerably more intensive than in water
Relation between the thicknesses of the viscous layer and the thermal boundary layer was established
Numerically predicted Nusselt numbers were in quantitative agreement with registered experimental laws
CONCLUSIONS
“FLOMANIA”, DES WORKSHOP, 2/3 July 2003, St.-Petersburg