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Giorgio CRASTO, Francesco PARAGGIO
giorgio.crasto@gmail.com
fparaggio@gmail.com
Third Symposium on OpenFOAM® in Wind Energy. Politecnico di Milano 15-17 June 2015
RANS Simulations of Askervein
hill with OpenFOAM®
The Askervein Hill project
• Askervein is a well known test-site where
extensive wind measurements were carried
out in ‘82 and ‘83.
• Is considered to be an Isolated hill
– Althought some other hills are close at NE ... Map
A and Map B are available (thanks to Prof. P.Taylor)
• Neutral stratification ... Run TU03-B
• Homogenous roughness? (z0 0.03m or what?)
2
• Map A: 257x257 – 16km x 16km => 62.5m
• Map B: 257x257 – 6km x 6km => 23.4375m
Askervein Hill: an isolated hill?
3
Askervein Hill: resolution consequences
4
• Askervein, a 116m high hill: Map A Map B
115.108m 116.837m
Askervein Hill: measurements points
• HT Hill Top
• CP Center Point
• RS Reference Site
• Line A through HT
• Line AA through CP
• Line B main axis
• TU03-B (210°)
5
Askervein Hill: homogeneous roughness?
6
Negligible?
Simulations 2D, rectangular domain
7
• Reynolds Averaged Navier-Stokes (RANS)
• Standard k-e turbulence model
• Effects of model constant se on the wall-
functions
• Periodic BC
– Mass flow given
0,000
0,005
0,010
0,015
0,020
0,025
0,030
0,035
0,040
0 5 10 15 20 25
z0obtainedbyinterpolationh/2-100m]
ratio first cell over roughness length (h/z0)
se 1.44
se 1.30
se 1.11
~11.8
Height of first (ground adjacent)
cell ~ 11.8 * 0.03m = 0.354m
3D simulations on a cubic domain
8
• The snappyHexMesh applied directly to the
orography of the site gave a poor quality grid.
terrainBlockMesher (TBM) + SHM
9
• snappyHexMesh only NO!
• terrainBlockMesher => boundary-fitted grid ok
• terrainBlockMesher + SNM ... More promising
• ZephyTOOLS prismatic cells over a cylindrical
domain (mesher M1)
TBM + snappyHexMesh
10
1. terrainBlockMesher (body-fitted)
2. 1° level snappyHexMesh
3. 2° level snappyHexMesh
PRO: reduced height first cell; increased resolution close to the ground
CON: expansion ratio 2, generally accepted <1.2
Further settings
• Standard k-e model
• simpleFoam (incompressible)
• First cell height 2m (= 66.67*z0) - not 0.354m!!
– Non-orthogonality alarms reducing the grid size
• Convergence criteria:
11
OF 2.3.1 default (for ABL test-case) ZephyTOOLS default
p 1e-3;
U 1e-4;
"(k|epsilon)" 1e-4;
p 5e-4;
U 1e-5;
"(k|epsilon)" 1e-5;
ZephyTOOLS
vref 15m/s
href 500m
CUBIC GRID
vref 16.016m/s
href 1008m
ut = 0.63 m/s
1 and 2 cells per sHM level (Speed)
12
1 and 2 cells per sHM level (TKE)
13
- 2 cells for each level
- More was not accepted by my and
the grid generated had only one
cell per level!
Discretization schemes (Speed)
14
Residuals:
p 5e-4
U 1e-5
"(k|epsilon)" 1e-5
Discretization schemes (TKE)
15
Residuals:
p 5e-4
U 1e-5
"(k|epsilon)" 1e-5
Discretization schemes
16
Discretization schemes
17/21
Discretization schemes and RMSE
map Grid generation Scheme (divSchemes) RMSerr. Speed RMSerr. TKE
A TBM + 2 levels of SHM bounded linearUpwind 1.239643 0.766631
B TBM + 2 levels of SHM bounded linearUpwind 1.253133 0.748267
A TBM + 2 levels of SHM b. skewCorrected linearUpwind 1.293558 0.781646
B TBM + 2 levels of SHM b. skewCorrected linearUpwind 1.309883 0.777852
A TBM + 2 levels of SHM b. linear (2nd ord. Central) 1.290942 0.899257
B TBM + 2 levels of SHM b. linear (2nd ord. Central) 1.474857 0.92132
A TBM + 2 levels of SHM bounded linearUpwindV 1.321186 0.799412
B TBM + 2 levels of SHM bounded linearUpwindV 1.350313 0.801742
TBM terrainBlockMesher
SHM snappyHexMesh
A ZephyTOOLS (OF 2.3.0) linearUpwind; upwind for k|e 0.993898 1.034235
B ZephyTOOLS (OF 2.3.0) linearUpwind; upwind for k|e 0.973765 0.995486
18/21
gradSchemes laplacianSchemes
TBM + 2l of SHM Gauss linear Gauss linear limited corrected 0.333
ZephyTOOLS cellMDLimited Gauss linear 0.5 Gauss linear limited 0.5
Speed [m/s]: TBM+SHM vs. ZephyTOOLS
19/21
TKE [m2/s2]: TBM+SHM vs. ZephyTOOLS
20/21
Conclusions & Future Steps
21
 Highlighted the grid sensitivity (vertical and horizontal)
 SHM not satisfying; TBM + SHM promising
 Need to improve the code to automize the gridding while
satisfing the h/z0 rule; some limits due to PC;
 No substantial difference between cubic and ZT in terms of
results (speed&tke) ... Probably differences due to the SHM
 ZT slightly underestimeted the speed-up at HT and the step
raise of TKE;
 Both methods understimated significantly the peak of TKE
(due to turbulence modelling?);
 Improve (automize) the gridding;
 Test cases with roughness maps (Bolund);
 Compute the production of a Wind Farm.

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crasto-paraggio

  • 1. Giorgio CRASTO, Francesco PARAGGIO giorgio.crasto@gmail.com fparaggio@gmail.com Third Symposium on OpenFOAM® in Wind Energy. Politecnico di Milano 15-17 June 2015 RANS Simulations of Askervein hill with OpenFOAM®
  • 2. The Askervein Hill project • Askervein is a well known test-site where extensive wind measurements were carried out in ‘82 and ‘83. • Is considered to be an Isolated hill – Althought some other hills are close at NE ... Map A and Map B are available (thanks to Prof. P.Taylor) • Neutral stratification ... Run TU03-B • Homogenous roughness? (z0 0.03m or what?) 2
  • 3. • Map A: 257x257 – 16km x 16km => 62.5m • Map B: 257x257 – 6km x 6km => 23.4375m Askervein Hill: an isolated hill? 3
  • 4. Askervein Hill: resolution consequences 4 • Askervein, a 116m high hill: Map A Map B 115.108m 116.837m
  • 5. Askervein Hill: measurements points • HT Hill Top • CP Center Point • RS Reference Site • Line A through HT • Line AA through CP • Line B main axis • TU03-B (210°) 5
  • 6. Askervein Hill: homogeneous roughness? 6 Negligible?
  • 7. Simulations 2D, rectangular domain 7 • Reynolds Averaged Navier-Stokes (RANS) • Standard k-e turbulence model • Effects of model constant se on the wall- functions • Periodic BC – Mass flow given 0,000 0,005 0,010 0,015 0,020 0,025 0,030 0,035 0,040 0 5 10 15 20 25 z0obtainedbyinterpolationh/2-100m] ratio first cell over roughness length (h/z0) se 1.44 se 1.30 se 1.11 ~11.8 Height of first (ground adjacent) cell ~ 11.8 * 0.03m = 0.354m
  • 8. 3D simulations on a cubic domain 8 • The snappyHexMesh applied directly to the orography of the site gave a poor quality grid.
  • 9. terrainBlockMesher (TBM) + SHM 9 • snappyHexMesh only NO! • terrainBlockMesher => boundary-fitted grid ok • terrainBlockMesher + SNM ... More promising • ZephyTOOLS prismatic cells over a cylindrical domain (mesher M1)
  • 10. TBM + snappyHexMesh 10 1. terrainBlockMesher (body-fitted) 2. 1° level snappyHexMesh 3. 2° level snappyHexMesh PRO: reduced height first cell; increased resolution close to the ground CON: expansion ratio 2, generally accepted <1.2
  • 11. Further settings • Standard k-e model • simpleFoam (incompressible) • First cell height 2m (= 66.67*z0) - not 0.354m!! – Non-orthogonality alarms reducing the grid size • Convergence criteria: 11 OF 2.3.1 default (for ABL test-case) ZephyTOOLS default p 1e-3; U 1e-4; "(k|epsilon)" 1e-4; p 5e-4; U 1e-5; "(k|epsilon)" 1e-5; ZephyTOOLS vref 15m/s href 500m CUBIC GRID vref 16.016m/s href 1008m ut = 0.63 m/s
  • 12. 1 and 2 cells per sHM level (Speed) 12
  • 13. 1 and 2 cells per sHM level (TKE) 13 - 2 cells for each level - More was not accepted by my and the grid generated had only one cell per level!
  • 14. Discretization schemes (Speed) 14 Residuals: p 5e-4 U 1e-5 "(k|epsilon)" 1e-5
  • 15. Discretization schemes (TKE) 15 Residuals: p 5e-4 U 1e-5 "(k|epsilon)" 1e-5
  • 18. Discretization schemes and RMSE map Grid generation Scheme (divSchemes) RMSerr. Speed RMSerr. TKE A TBM + 2 levels of SHM bounded linearUpwind 1.239643 0.766631 B TBM + 2 levels of SHM bounded linearUpwind 1.253133 0.748267 A TBM + 2 levels of SHM b. skewCorrected linearUpwind 1.293558 0.781646 B TBM + 2 levels of SHM b. skewCorrected linearUpwind 1.309883 0.777852 A TBM + 2 levels of SHM b. linear (2nd ord. Central) 1.290942 0.899257 B TBM + 2 levels of SHM b. linear (2nd ord. Central) 1.474857 0.92132 A TBM + 2 levels of SHM bounded linearUpwindV 1.321186 0.799412 B TBM + 2 levels of SHM bounded linearUpwindV 1.350313 0.801742 TBM terrainBlockMesher SHM snappyHexMesh A ZephyTOOLS (OF 2.3.0) linearUpwind; upwind for k|e 0.993898 1.034235 B ZephyTOOLS (OF 2.3.0) linearUpwind; upwind for k|e 0.973765 0.995486 18/21 gradSchemes laplacianSchemes TBM + 2l of SHM Gauss linear Gauss linear limited corrected 0.333 ZephyTOOLS cellMDLimited Gauss linear 0.5 Gauss linear limited 0.5
  • 19. Speed [m/s]: TBM+SHM vs. ZephyTOOLS 19/21
  • 20. TKE [m2/s2]: TBM+SHM vs. ZephyTOOLS 20/21
  • 21. Conclusions & Future Steps 21  Highlighted the grid sensitivity (vertical and horizontal)  SHM not satisfying; TBM + SHM promising  Need to improve the code to automize the gridding while satisfing the h/z0 rule; some limits due to PC;  No substantial difference between cubic and ZT in terms of results (speed&tke) ... Probably differences due to the SHM  ZT slightly underestimeted the speed-up at HT and the step raise of TKE;  Both methods understimated significantly the peak of TKE (due to turbulence modelling?);  Improve (automize) the gridding;  Test cases with roughness maps (Bolund);  Compute the production of a Wind Farm.