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Turbulence model and numerical scheme assessment for buffet computations
Eric Goncalvès da Silva, Robert Houdeville
To cite this version:
Eric Goncalvès da Silva, Robert Houdeville. Turbulence model and numerical scheme assessment for buffet computations. International Journal for Numerical Methods in Fluids, Wiley, 2004, 46 (11), pp.1127-1152. �10.1002/fld.777�. �hal-00530301�
Assessment for Buet Computations
Eri GONCALVES
LEGI
BP 53,38041 Grenoble edex 9,Frane
Eri.Gonalveshmg.inpg.fr
Robert HOUDEVILLE
ONERA-Toulouse, Departmentof Aerodynamis and Energetis,
BP 4025, Toulouse, 31055edex, Frane
Robert.Houdevilleoneert.fr
Abstrat
The preditionof shok-indued osillationsovertransoni rigid airfoilsisimportant for a
betterunderstandingofthebuetingphenomenon. TheunsteadyresolutionoftheNavier-
Stokesequations isperformedwithvarioustransport-equation turbulenemodelsinwhih
orretionsareaddedfornon-equilibriumows. Thelakofnumerialeienyduetothe
CFL stabilityonditionisirumventedbytheuseofawalllawapproah andadualtime
steppingmethod. Moreover,variousnumerialshemesareusedtotryandbeindependent
of thenumerial disretization.
ComparisonsaremadewiththeexperimentalresultsobtainedforthesuperritialRA16SC1
airfoil. TheyshowtheinterestinusingtheSSTorretionorrealizabilityonditionstoget
orretpreditions ofthefrequeny,amplitude and pressureutuations overtheairfoil.
Keywords
Buet, Unsteady Flows, Turbulene Modelling,Numerial Sheme
x, y, z loalwall frame (boundarylayer) Uτ fritionveloity
Cf shearstress oeient Cp pressureoeient
Fc, Fd onvetive and diusiveux densities Pk turbulent kineti energy prodution M∞ innite Mahnumber
Rec Reynoldsnumberbased onthemean hord Ti stagnationtemperature
u, v, w veloityomponentsinthe loalwall frame q total heatux,qv+qt
k turbulent kineti energy P statipressure
Pr, Prt Prandtl numbers
T meanstatitemperature
α angleof attak ε dissipationrate
κ von Karmanonstant ω speidissipation
µ, µt moleular andeddy visosity
ρ density
τ total stresstensor, τv+τt
w wall value
+ wall sale
1 adjaent ell withrespetto the wall v
visous
t
turbulent
The numerial simulation of unsteadyturbulent ows around airfoilsis motivatedbythe
need to better understand omplex owphenomena appearing inaeronauti appliations
suh as ows overairraft wings. Thepresent work fouses on the transonibuet. This
aerodynamiphenomenonresultsinaself-sustainedperiodimotionoftheshokwaveover
the surfae of the airfoil, due to the development of instabilities ausedby theboundary
layerseparationandtheshokwaveinteration. Theshok-induedosillations(SIO)over
rigid airfoils in transoni regime have been lassied by Tijdeman for fored instabilities
using a moving trailing edge ap [1℄. A detailed desription of the physial features of
SIOisgivenbyLee [2℄. Thisproblemisofprimaryimportane foraeronautiappliations
as it an lead to the bueting phenomenon through the mehanial response of the wing
struture. The large amplitude periodi variation of lift assoiated withbuet limitsthe
ruisingspeedofommerial airraftandseverelydegradesthemaneuverabilityofombat
airraft. Aurate preditionsofsuh ow phenomenais ofsignianttehnologial inter-
estandtheirsimulationremainsahallengingproblemduetotheomplexphysisinvolved.
Today, despite the fast improvement of omputer performanes, the unsteady resolu-
tion of the Navier-Stokes equations remains a diult problem. Three-dimensional time-
dependent omputations obtained with large eddy simulations (LES) and espeiallywith
diretsimulations (DNS) arenot yetpratial for this kind ofappliations beause ofthe
highdemands inomputerresoures. Inthisstudy,theReynoldsdeompositionwasused
withanaveragedstatistialproessingresulting intheRANSequationsfor themeanow
quantities. Thisapproah leads to alowfrequeny separation between modeledand om-
puted sales. It is well known that these equations an be legitimely used for ows in
whih thetime sale ofthe meanowunsteadiness ismuh larger than theharateristi
timesaleofthe turbulene. Thisistheasewiththetransonibuetinwhihtheshok-
indued osillation frequenyis around100Hz.
TheReynoldsdeompositionintroduesadditionalunknownquantitiesliketheReynolds
stress tensor and requires a turbulene model to lose theequation system. Various tur-
bulene losures an be found in the literature of unsteady numerial simulation ows
assoiatedwithbuet,osillatingairfoilsordynamistall. Modelsaremoreor lesssophis-
models [5, 6, 7, 8, 9℄, to EARSM [8℄, RSM [9℄ and non-linear models [9℄. Regarding the
shok loation for steady ows, algebrai models annot give preditions withan aept-
ablelevelofauray. Thestandard eddy-visositymodelsbasedonthelinearBoussinesq
relation are known to be aited by numerous weaknesses, inluding seriously exessive
generationofturbuleneatimpingement zones, aninabilityto apturetheboundarylayer
separation andaviolationofrealizabilityat largerates ofstrain. Moreover,thesesmodels
are formulated following thespetral energy of Kolmogorov withan equilibrium assump-
tion of turbulene and they are alibrated for steady ows. However, for unsteady ows,
the preseneof oherent strutures an break this equilibriumand lead to a dierent en-
ergydistribution. Anobservedonsequeneistheover-produtionofeddy-visosity,whih
limits the unsteadiness development and modies the ow topology. The present study
investigated some orretionsfor standard linearmodels suhastheshear stree transport
(SST) Menter orretion and the use of realizability onstraints. A rst study was on-
duted,onsistingofnumerialsimulationoftransonibuetoverairfoils[10 ℄withtheSST
orretion. It were shown the great inuene of this limiter for two-equation models and
goodresults wereobtained. Otherwaysoflimitingtheeddy-visosityortheprodutionof
turbulenekinetienergyanbeused,suhasadereasethevalueoftheCµoeient[12℄
or theintrodution of thevortiityintheprodution term [13℄but they werenot tested.
Another important aspet onerns the numerial methods and the omputer ost.
Indeed,unsteadyRANSomputationswithturbulenemodelsremainexpensive. Expliit
methods solved the equations using a global timestep omputed as the minimum of the
loal time step assoiated with eah grid ell. The CFL stability riterion drastially
redues the method eieny for ne meshes for whih the dimensionless mesh size at
the wall must be of unity order, in wall units. To overome this diulty, a wall law
approah isusedto relaxthe meshrenement nearthewall[11 ℄. Moreover,omputations
areperformedwithaneientimpliitmethodallowingsomelargetimestepsandwiththe
dualtime-steppingapproahallowingtheuseofaelelerationtehniquessuhasmultigrid
algorithm andloaltimestep. Finally,the paperpresentsanumerial sheme omparison
to study the inuene of the sheme on these unsteady omputations and to try and be
independent of thespatial disretization.
Thenumerial simulationswerearriedoutusinganimpliitCFDodesolvingtheunou-
pled RANS/turbulent systems for multi-domain strutured meshes. This solver is based
on aell-entered nite-volume disretization.
2.1 Governing equations
The ompressible RANS equations oupled with a two-equation turbulene model in in-
tegral form are written for a ell of volume Ω limited by a surfae Σ and with an outer
normaln. Theseequations an be expressedas: d
dt Z
Ω
w dΩ + I
Σ
Fc.n dΣ− I
Σ
Fd.n dΣ = Z
Ω
S dΩ (1)
w=
ρ ρV ρE
ρk ρΨ
; Fc =
ρV ρV ⊗V +pI
(ρE+p)V ρkV ρΨV
; Fd=
0
τv+τt (τv+τt).V −qv−qt
(µ+µt/σk)gradk (µ+µt/σΨ)gradΨ
where w denotes the onservative variables, Fc and Fd the onvetive and diusive ux
densities and S the soure terms whih onern only the transport equations. Ψ is the
length sale determiningvariable.
The exatexpressionof the eddyvisosityµt andthesoure termsdependsontheturbu-
lene model, aswell astheonstants σk and σΨ.
The total stress tensor τ is evaluated following the Stokeshypothesisand the Boussinesq
assumption. ThetotalheatuxvetorqisobtainedfromtheFourierlawwiththeonstant
Prandtl numberhypothesis.
τ = τv+τt= (µ+µt) 1
2(gradV + (gradV)t)−2
3(divV)I
+ 2
3kI (2) q = qv+qt=−
µ Pr + µt
Prt
CpgradT (3)
For the mean ow, the spae-entered Jameson sheme [14 ℄ was used. It was stabilized
by a salar artiial dissipation onsisting of a blend of 2
nd
and 4
th
dierenes. For the
turbulene transport equations, the upwind Roe sheme [15 ℄ was used to obtain a more
robust method. The seond-order auray was obtained by introduing a ux-limited
dissipation [16 ℄. The Harten'sentropy orretionwasused.
Time integration was performed through a matrix-free impliit method [17, 18℄. The
impliit method onsists in solving a system of equations arising from the linearization
of a fully impliit sheme, at eah time step. The main feature of this method is that
thestorage of the Jaobian matrix is ompletely eliminated, whih leads to a low-storage
algorithm. The visous ux Jaobian matries are replaed by their spetral radii. The
onvetive ux are written withthe Roe sheme instead of the Jameson sheme beause
of thedissipationterm, theuseof aninonsistentlinearization having no onsequene for
steady omputations. The Jaobian matries whih appear from the linearization of the
entered uxes areapproximated with thenumerial uxes and thenumerial dissipation
matriesare replaedbytheir spetralradii.
Conerning theturbulenetransportequations,thediusive uxJaobian matrixarealso
replaedbytheir spetralradii. Thesoure termneeds aspeialtreatment [19 ℄. Onlythe
negativepartofthesouretermJaobian matrixisonsideredandreplaedbyitsspetral
radius.
The impliittime-integration proedure leadsto a systemwhihan besolveddiretly or
iteratively. Thediretinversion an be memory intensive and omputationally expensive.
Therefore, an impliit relaxation proedure is preferred and the point Jaobi relaxation
algorithm washosen.
For steady state omputations, onvergene aeleration was obtained using a loal
timestep and the fullapproximation storage(FAS)multigrid methodproposed byJame-
son[20 , 21℄. Foring funtionsaredened ontheoarsergrids and added totheresiduals
usedforthesteppingsheme. Theorretionsomputedoneahoarsegridaretransferred
bak to the ner one by trilinear interpolations. Theturbulent equations areonly solved
onthenegridandthe omputededdyvisosityµt istransferred totheoarsegrids. The
Forunsteadyomputations,thedualtimesteppingmethod,proposedbyJameson[21℄,
was used to takle the lak of numerial eieny of the global time stepping approah.
The derivative withrespetto thephysial timeis disretized bya seond-order formula.
Making the sheme impliit with respet to the dual time provides fast onvergene to
the time-aurate solution. Between eah time step, the solution is advaned in a dual
time and aeleration strategies developed for steady problems an be used to speed up
the onvergene intitious time. The initialization of the derivative withrespetto the
physial time wasperformedwitharst-order formula.
2.3 Far eld onditions
At the outer edge ofthe omputational domain,a non-reeting onditionis used witha
vortiityorretion inorderto simulateauniform inniteow. Itisdeduedfromtheow
eld induedby asingle vortex,thestrength ofwhih isgivenbytheairfoil lift[22 ℄.
2.4 Turbulene Models
Various popular two-equation turbulene models were used in the present study : the
Smith k−l model [23 , 24 ℄, the Wilox k−ω model [25℄, the Menter SST k−ω model
[26 , 27℄, the high Reynoldsversion ofthe Jones-Launder k−εmodel [28 ℄,theKokk−ω
model [29℄and also theone-equationSpalart-Allmaras model [30,31℄.
Asthedisretizationshemedoesnotinsurethepositivityoftheturbulentonservative
variables,limiterswereusedto avoidnegativekorΨvalues. Theselimiters weresetequal
to theorresponding imposedboundary values inthe far eld.
SST orretion
The Menter orretion is basedon the empirial Bradshaw'sassumption whih bindsthe
shear stress to the turbulent kineti energy for two-dimensional boundary layer. This
orretion was extendedforthe k−εmodeland the k−lmodel.
The nonequilibrium orretion of Smith [32℄, developed for the k−l model, onsists in
modifying the omputationof the eddy visositybyintroduinga funtion σ : µt=σµteq ; σ= α−0.25α1/2+ 0.875
α3/2+ 0.625 ; α= min Pkeq,0
ε (4)
where the subsript eq denotes the equilibrium value. The non-equilibrium funtion was hosen to limit the eddy-visosity when prodution is greater than dissipation and to in-
rease thevisosityabove theequilibriummodelvalueintheontraryase.
Durbin orretion - link with realizability
Based on the realizability priniple (the variane of the utuating veloity omponents
shouldbepositive andtheross-orrelationsboundedbytheShwartzinequality), amini-
mal orretionwasderivedfor two-equation turbulenemodelsandwasshownto urethe
stagnation-pointanomaly[33℄. Theonditiontoensurerealizabilityinathree-dimensional
owis:
Cµ≤ 1 s√
3 ; s= k
εS ; S2 = 2SijSij −2
3Skk2 (5)
A weakly non-linear model was thus obtained [35℄ with a Cµ oeient funtion of the
dimensionless meanstrainrate :
Cµ= min
Cµo, c s√
3
with c≤1 (6)
where Cµo is settothe onstant value0.09. Durbin xedthevalueoftheonstantc to0.5
for good results inimpinging jets [34 ℄. Then, the following relation wasobtained for the
k−εmodel:
µt=ρCµk2
ε ; Cµ= min
Cµo,0.3 s
(7)
And for the k−ω model:
µt=ρCµk
ω ; Cµ= min
1, 0.3 Cµos
(8)
ItshouldbenotedthatthisorretionissimilartotheSSTformulabyreplaingΩwith S. Yet, the Durbin orretion is established with mathematial onepts and is available
for three-dimensional ows whereas the SST orretion is based on an empirial two-
dimensionalhypothesis. Thismodelhasbeensuessfullytestedonshokwave/boundary
layer interations withthe Wilox k−ω model[35 ℄.
The Kokmodel hasbeen builtin orderto resolve thedependeneon freestreamvalues of
ω. Theturbulene transport equations ofthemodelare given by:
∂ρk
∂t + div[ρkV−(µ+σkµt)gradk] = Pk−β∗ρkω
∂ρω
∂t + div[ρωV−(µ+σωµt)gradω] = Pω−βρω2 +σdρ
ω gradk.gradω
Kok obtained additionalonstraintsfor theonstants:
σω−σk+σd>0 σk−σd>0
The hoie of Kokwas:
σω = 0.5 ; σk= 2/3 ; σd= 0.5
Theonstant values were hanged, following all onstraints, to showthesensitivityof
the modelto the ross-diusion term gradk.gradω intheω equation for these unsteady
omputations.
test 1: σω = 0.5 ; σk = 2/3 ; σd = 0.65
test 2: σω = 0.5 ; σk = 1 ; σd = 0.85
2.5 Wall law approah
At the wall, a no-slip ondition was used oupled to a wall law treatment. It onsistsin
imposingthe diusiveuxdensities, requiredfor theintegration proess,inadjaent ells
to a wall. Theshear stress τ and theheatuxq areobtained from an analytialveloity
prole :
u+ = y+ if y+<11.13
u+ = 1
κlny++ 5.25 if y+>11.13 u+ = u/Uτ ; y+= yUτ
νw
(9)
In equation(9), urepresentsthevanDriest [36,37 ℄ transformed veloity forompressible ows.
Conerningtransport-equationturbulenemodels,kwassetto0atthewallanditspro-
dutionwasimposedaordingtotheformulationproposedbyViegasandRubesin[38 ,39℄.
Theseond variablewasdeduedfromananalytial relationandwasimposedinadjaent
ells to a wall. The harateristi length sale of the Chen model [40℄ was used for the
dissipation rate εand the spei dissipation ω. For theSmith model, a standard linear
law forthe lengthl wasused.
For the one-equation Spalart-Allmaras model, the transported quantity was imposed in
adjaent ellstoawallbyusingthe losurerelations ofthemodel,theveloityproleand
a mixing-length formulation for the eddy-visosity. Moredetails onerning thewall law
approah aregiven in[11℄.
For unsteady boundary layers, the existene of a wall law was assumed valid at eah
instant. As shown in [41 ℄, the veloity phase shift is nearly onstant in the logarithmi
region and equal to the shift of the wall shear stress phase. This is true for a Strouhal
numberup to 10.
Whenusingthewalllawapproahwiththemultigridalgorithm,thewalllawboundary
ondition wasappliedon the negridand theno-sliponditionwasapplied on theoarse
grids.
3 Numerial results
3.1 Experimental onditions
The experimental study was onduted inthe S3MA ONERA wind tunnel [42 ℄ withthe
RA16SC1 airfoil. It is a superritial airfoil with a relative thikness equal to 16% and
a hord length equal to 180mm. The RMS pressure utuations were measured from 36 Kulite transduers installed in the airfoil. The ow onditions were : M∞ = 0.732, Ti = 283K, Rec = 4.2 106 and the angle of attak varied from 0 to 4.5◦. Transition was
xed nearthe leading edgeat x/c= 7.5%on both sidesof theairfoil.
For the omputations, experimental orretions were used. The Mah number was de-
reased by0.09 and the angleofattakwasdereasedby1◦ at allinidenes withrespet
to experiment. ThegridwasaC-typetopology. Itontained 321×81 nodes,241 ofwhih
were on the airfoil(f. gure1,2). They+ values ofthe oarse mesh,at theenter ofthe
rst ell,arepresentedingure3 for asteady omputation atα= 4◦.
Thenumerial parameters usedfor the omputationswere :
- thedimensionless time step, ∆t∗ = ∆tai c = 0.2
where c isthe hord ofthe airfoiland ai the stagnation soundveloity
- grid levels for themultigrid method,2
- sub-iterationsof thedualtime steppingmethod,75 upto 100
By inreasing the number of sub-iterations, it was heked that the same solution was
ahieved.
- theCFL number, 200
- Jaobi iterationsfor the impliit stage,14
- the artiial dissipation of the Jameson sheme introdues two oeients, one for the
seond-dierene term: χ2 = 0.5 and one for the fourth-dierene term: χ4 = 0.016. For
theseond gridlevel, theoeient χ4 wasxedat 0.032
- theoeient of the Harten'sorretion, 0.05
Computations started from a uniform ow-eld using a loal time step and one grid
level. After 50 iterations, the dual time stepping method was used with the mulgrid
algorithm and osillationsdevelopwitha growing amplitude.
3.3 Comparison of turbulene models
The frequeny f and theamplitude of the lift oeient ∆CL arereportedin table 1 for
all turbulenemodels and forthree angles ofattakα= 3,4and 5◦,orresponding tothe buet onset, established phenomenon and buet exit, i.e. the return to a steady state,
respetively.
The apaity of turbulene models to restitute the natural unsteadiness of the ow