under Laminar Conditions with
Detailed Chemistry
Vom Fa hberei h Mas hinenbau
an der Te hnis hen Universität Darmstadt
zur
Erlangung des Grades eines Doktor-Ingenieurs (Dr.-Ing.)
genehmigte
D i s s e r t a t i o n
vorgelegt von
Dipl.-Ing. Jesús Contreras Espada
aus Librilla (Spanien)
Beri hterstatter: Prof. Dr.Ing. J. Jani ka
Mitberi hterstatter: Prof. Dr. rer. nat. M. S häfer
Tag der Einrei hung: 3. November 2009
Tag der mündli hen Prüfung: 8. Dezember 2009
Darmstadt 2010
Manypeoplehavehelpedmeinthe ourseofmyresear hinwritingthisbook,andanymerit
in it is inlarge measure due to them. First and foremost, I gladly a knowledge my debt to
Prof.Dr.-Ing. Johannes Jani kaoftheTe hni al UniversityofDarmstadtwhoinvitedmeto
be omeamemberofhisteamand whowas mytea her andsupervisor inthiswork. I thank
himforhisex ellentandtirelessguidan e,en ouragementandpatien ethroughouttheyears
of the study. I alsowanttothank Prof.AmsiniSadikiforprovidingmeassistan e and good
advi e duringall my years inDarmstadt, andfor helpingshapepapers and presentationsin
so many o asions. I thank Dr. Andreas Dreizler forhis remarks and helpful dis ussions.
Tomy olleagues,who madeour departmentanidealpla e toworkatandwho gaveme
all the explanations, suggestions and en ouragement that I required from them, and even
more: Rajani Kumar Akula, Mouldi Chrigui, Dmitry Goryntsev, Alex Maltsev, Bernhard
Wegner,Eri hWa hter,ZdravkoStojanovi ,AndreasKempf,Mi haelDüsing,JanBrüba h,
Bern Groh, Frederik Hahn, Clemens Olbri h, Desislava Dimitrova, Elena and Christoph
S hneider, MartinFreitag,Mi haelHage, YingHuai,ThomasKania,BenjaminBohm,Mar
Aurel Gregor,SunilOmar,RangaReddy Kottam,AndreasNauert,FelixFlemming,Florian
Serin, Dirk Geyer and Markus Klein, who rst invited me to EKT in the name of Prof.
Jani ka.
Thanks toPetra Knopand Elizabeth Zweyrohn for theireveryday help. They made my
work easier be ause I ould on entrate on it while they were worrying about everything
else.
Andoutsideourinstitute, thankstoTakeshi Omori,MiklosKanzamar,KristjanHorvat,
Christof Sodtke and Sanjin Sari for their friendship and en ouragement. Thanks to Prof.
Markov and Ri ard Consul for helping ll my gaps in ombustion modeling and numeri al
methods, and thanks to Ursula Kleins hmidt and Monika Thom who helped me with my
language skills.
The thesis was mostly written within the framework of the Graduiertenkolleg
'Model-lierung und numeris he Bes hreibung te hnis her Strömungen'. The graduate programwas
generously nan ed by the Deuts he Fors hungsgemeins haft.
And nally and most espe ially I would like to thank my parents, who made a great
eort to provide me with advantages they never had, I oer my deepest appre iation and
gratitude.
I de lare that this thesis does not in orporate without a knowledgement any material
previously submitted for a degree or diploma in any university and that to the best of my
knowledgeitdoesnot ontainany materialspreviously publishedorwrittenbyanother
per-son ex ept where due referen e is made inthe text.
Nomen lature vi
1. Introdu tion 1
1.1. Motivation and aimof the present work. . . 1
1.2. Combustionresear h . . . 2
1.3. Literature overview . . . 4
1.4. Codes used inthis work . . . 5
1.4.1. The FASTEST-3D ode . . . 5
1.4.2. The CHEMKIN-Pa kage . . . 5
1.4.2.1. CHEMKIN (Kee, Rupley and Miller,1989) . . . 5
1.4.2.2. SENKIN (Lutz, Kee and Miller,1988) . . . 5
1.4.2.3. PSR (Glarborget al.,1986) . . . 6
1.4.3. The FLUENT ode . . . 7
1.5. Content des ription . . . 8
2. Fundamentals 10 2.1. The Navier-Stokes equations . . . 10
2.2. The energy equation . . . 10
2.3. The spe ies transportequations . . . 12
2.4. An introdu tionto hemi al kineti s . . . 13
2.4.1. Chemi al Me hanisms . . . 14
2.4.2. Me hanism redu tion methods . . . 14
2.4.2.1. Equilibrium Chemistry . . . 14
2.4.2.2. Quasi Steady State Assumption . . . 15
2.4.2.3. ILDM-Model . . . 16
2.5. CombustionTheory . . . 17
2.5.1. Nitrogen rea tions . . . 18
2.5.2. Ex ess airand air fa tor . . . 18
2.5.3. LowMa h number ombustion. . . 19
2.6. Numeri alMethods . . . 20
2.6.1. The nite-volume method . . . 20
2.6.1.1. Surfa e integrals . . . 21
2.6.1.2. Volume integrals . . . 22
2.6.1.3. Deferred orre tion . . . 22
2.6.2. The SIMPLE algorithm . . . 22
2.6.3. The SIP-solver . . . 27
2.6.4. Rhie-Chow Velo ity Interpolation . . . 28
2.6.6. The Operator-Splittingmethod . . . 31
2.6.6.1. Operator-Splittingpro edures . . . 31
2.6.6.2. Errors of the method . . . 34
3. 1-D Simulations 35 3.1. Stoi hiometri
H
2
− air
ombustion . . . 373.1.1. Simulationof the perfe tlystirred rea tor onguration . . . 39
3.1.2. Simulationof the plug-owrea tor onguration. . . 39
3.2. Stoi hiometri
CH
4
− air
ombustion . . . 453.2.1. Simulationof the plug-owrea tor onguration. . . 46
4. 2D-Simulations 51 4.1. Hydrogen Combustion . . . 52
4.1.1.
H
2
Mi ro-Combustor . . . 524.1.1.1. Conguration understudy . . . 52
4.1.1.2. Simulationresults . . . 53
4.1.2.
H
2
Bunsen Burner . . . 624.1.2.1. Conguration understudy . . . 62
4.1.2.2. Simulationresults . . . 63
4.2. Methane Combustion . . . 72
4.2.1. Cold WallStabilized Methane Flame . . . 72
4.2.1.1. Conguration understudy . . . 72
4.2.1.2. Simulationresults . . . 73
4.3. Flameswith variabledensity . . . 82
4.3.1. EKT Standard Burner . . . 82
4.3.1.1. Conguration understudy . . . 82
4.3.1.2. Simulationresults . . . 83
5. Con lusions and Perspe tive 91 A. Rea tion me hanisms 95 A.1.
H
2
Combustion Me hanism . . . 95A
Area (m2
)
φ
Equivalen e ratio (dimensionless)Ω
Angular velo ity;Ω
ij
, Mean rate of rotation tensor(s−1
)
~a
A eleration (m/s2
)
a
Lo alspeed of sound (m/s)c
Con entration (mass/volume, moles/volume)c
p
,c
v
Heat apa ity at onstant pressure, volume (J/kg-K)D
ij
, D
Mass diusion oe ient(m2
/s)
E
Totalenergy, a tivationenergy (J,kJ, al)~g
Gravitational a eleration(m/s2
)
H
Totalenthalpy (energy/mass, energy/mole)h
Heat transfer oe ient(W/m2
-K)
h
Spe ies enthalpy (energy/mass, energy/mole)h
0
Standard state enthalpy of formation(energy/mass, energy/mole)
J
Mass ux; diusion ux (kg/m2
-s)
K
Equilibrium onstant = forward rate onstant/ba kward rate onstant (units vary)k
Rea tionrate onstant,e.g.,k
1
,k
−1
,k
f,r
,k
b,r
(units vary)k
B
Boltzmann onstant(1.38 × 10
−23
J/mole ule-K)
k
,k
c
Mass transfer oe ient (unitsvary);alsoK
,K
c
ℓ, l, L
Length s ale (m) Le Lewis numberm
Mass (kg)˙
m
Mass owrate (kg/s)M
w
Mole ular weight (kg/kgmol)M Ma h number
Nu Nusselt number
p
Pressure (Pa) Pe Pe let numberPr Prandtl number
Q
Flowrate of enthalpy (W)q
Heat ux(W/m2
)R
Gas-law onstant (8.31447× 10
3
J/kgmol-K)r
Radius (m)r
f
Forward rea tionrate (units vary)r
r
Reverse rea tionrate (units vary) Ra Rayleigh numberRe Reynolds number
S
Totalentropy (J/K, J/kgmol-K)s
Spe ies entropy;s
0
S S hmidt number
S
ij
Mean rate-of-strain tensor (s−1
)T
Temperature(K)t
Time (s)u, v, w
Velo ity magnitude (m/s)V
Volume(m3
)~v
Overall velo ity ve tor (m/s)X
k
Molefra tionY
k
Mass fra tion Greek lettersα
Thermaldiusivity(m2
/s)β
Coe ient of thermalexpansion (K−1
)
γ
Ratio of spe i heats,p
/v
∆
Change invariable, nal−
initialδ
Delta fun tion (unitsvary)ǫ
Lennard-Jones energy parameter (J/mole ule)ǫ
Turbulent dissipation rate (m2
/s
3
)
λ
Thermal ondu tivity (W/m-K)µ
Dynami vis osity ( P, Pa-s)ν
Kinemati vis osity (m2
/s)ν
′
,ν
′′
Stoi hiometri oe ients forrea tants, produ ts
ρ
Density (kg/m3
)σ
Stefan-Boltzmann onstant (5.67×10
8
W/m2
-K4
)τ
Shear stress (Pa)1.1. Motivation and aim of the present work
Heterogeneousrea tionsarethoseinwhi htwoormorephasesareinvolved. Alargenumber
of environmentallyand te hnologi allyimportantpro esses are based on hemi al rea tions
o urring at a surfa e. Heterogeneous atalysis, hemi al vapor deposition, orrosion,
ad-hesion, ozone depletion, ele tro hemistry: all of these phenomena have in ommon the fa t
that they require a hemi ally rea tive surfa e and a ow that arries the rea tants to the
rea ting zone. This ow orresponds, in many appli ations, to a gas mixture of dierent
spe ies.
For both e onomi and environmental reasons, onstant improvement in design and
optimizationofpro esseshasbe omemoreandmoreimportantovertime. Thisimprovement
requires a detailed knowledge of the lo al ow behavior and the multiphase phenomena.
Computational uid dynami s and hemi al kineti s an be inter onne ted to provide the
required knowledge for the improvementof heterogeneous pro esses.
The aim of this proje t is the modellingand simulation of omplex ongurations
pre-senting heterogeneousrea tions. Duetotheextensives opeofthe subje t,thisworkfo uses
on the hemi al rea tions in the gas phase. The implementation of a detailed hemistry
algorithmin a 3D CFD- ode has been a hieved through the ouplingof the CFD- ode and
a hemi al kineti s solver, whi h provides the produ tion/ onsumption rates of the spe ies
involved and the temperature hanges in the ontrol volumes, as well as some basi values
in these typesof simulations like transport oe ientsor vis osity of the dierent spe ies.
A Strang-like operator-splitting te hnique has been introdu ed in order to simplify the
problem, redu e the omputational time and avoid the drawba ks of sour e terms in the
spe ies and enthalpy equations. Two disadvantages, whi h are intrinsi to the method of
operator-splitting,arethe reationofdis ontinuitiesofthespatial on entrationdistribution
at the beginning of ea h ' hemi al' time step and splitting errors, whi h add up to the
dis retization errors and other errorsdue tothe numeri al solutionmethod.
One of the biggest advantages of this pro edure is, that it allows the simulation of
any kind of rea ting ow without having to perform big hanges in the ode. This high
exibility is a hieved through the separation ofthe owand hemistry solvers. In addition,
hemi al me hanism. Another advantage of this pro edure is the possibility of applying it
to turbulentows, multiphase and many other more omplex ongurations.
1.2. Combustion resear h
Combustionisnowadaysthemost importantformof energy onversion. Itisusedin
numer-ous pra ti alappli ationsinordertogenerateheat(industrialandhouseburners),ele tri ity
(heat power plants, gas turbines), for transport purposes (motors, turbines, rea tors) and
the destru tion of waste (in inerating plants). Combustionis hara terized by the
develop-ment of stronglyexothermi irreversible hemi alrea tions between afuel and a omburent
a ording to the followingglobal rea tion:
F uel + Oxidizer → P roducts + Heat
The heat release takes pla e generally in a very thin zone alled the ame front
(typ-i al values of this front are in the range of one millimeter or tenth of millimeter), whi h
an introdu e extremely high temperature and mass gradients and strong variationsof the
density in very small s ales. In ontrast to this, fuel ells onvert the hemi al energy of
an oxidation pro ess, known as old ombustion [29℄, dire tly into ele tri al energy with
lower emissionsand higher e ien y than internal ombustion engines[76℄. The maximum
membranetemperaturefor aLTFC(lowtemperaturefuel ell) isapproximately
80
◦
C
[9℄. A
large variety of fuels,gas, liquidorsolid, an be used: oal, wood, arbohydrates (methane,
butane, propane, gasoline, gasoil, kerosene...), hydrogen, ... The oxidizer is generally air
oxygenor,o asionally,pureoxygen( ertainindustrialfurna es, ro ketmotors)that allows
higher temperatures and avoids the storageand manipulation of nitrogen.
Combustion isa ombinationof several omplex, inter onne ted pro esses. The kineti
s hemes determine thefuel onsumptionrate andthe formationof produ tsand pollutants.
They are alsoimportant inthe pro esses ofignitionand extin tion ofthe ames. The mass
transfer of hemi al spe ies through mole ular diusion or onve tive transport is another
very important element of the ombustion pro ess. The heat release due to hemi al
rea -tionsintrodu esintenseheattransferthrough ondu tion, onve tionandradiationinsidethe
ow where ombustion takes pla e, but alsoin the environment (burner walls,et ...). This
thermalenergymustbeimmediatelyused eitherdire tlyorafter onversionintome hani al
energy in gas turbines orpiston engines. The des ription ofthe ow isrequired ingas
om-bustion. Inother systems thereare additionalpro esses that have tobe taken intoa ount:
two (liquid fuel) or three (solid fuel parti les) phases an be involved in the ombustion
pro ess, phenomena like vaporization, drop ombustion, et . must be taken into a ount,
sootformationisavery di ultproblemwhi hin ludes, generation,growth, aggregationof
Chemical T ime Scales
F isical T ime Scales
10
−8
s
10
−6
s
10
−4
s
10
−2
s
10
0
s
Slowtimes ales
forex. NOgeneration
frozenrea tions
Intermediate
times ales
Fast times ales
equilibriumrea tions
(quasisteadystate,
equilibrium)
Times alesfor
onve tionanddiusion
Equilibriumassumption
justied
Figure 1.1.: (From Warnatz[98℄) Comparison of hemi aland me hani als ales involved in
the ombustionpro ess
One of the main di ulties in the numeri al simulation of ombustion, apart from the
omplexityof the phenomena involved, liesin the bigrangeof time and lengths ales
orre-sponding to the dierent pro esses (see g. 1.1). Certain hemi al rea tions an take pla e
in very small domains (hundredths of millimeter) and very short periods of time (
10
−6
to
10
−10
se onds) while the burner an be several meters long (industrial furna es) and the
residen e times an be up to ten se onds or even longer. The predi tion of pollutants
re-quires the estimationof hemi al spe ies presentin part permillion(ppm), fa ingthe main
spe ies (oxygen, nitrogen, fuel, water vapor, arbon dioxide...) where the on entration is
more than thousand times higher.
The obje tiveof resear hin ombustionistoa hieveabetter understandingofthe
om-plexphenomenainvolved,inordertobeabletomodelandreprodu ethesephenomena. One
ofthenalgoalsisthe numeri alsimulationofindustrialsystemsorreal ongurations. The
development osts asso iated with a new prototype an be redu ed if numeri alsimulation
an be used to optimizethe burner before its onstru tion. This optimization an be done
a ording to dierent riteria: e ien y, pollutants, et . It an also help to avoid
insta-bilities in the ombustion. In addition to better understanding of the me hanisms, these
al ulations allowthe formationof databases used as models for turbulentows.
Numerous studies are related to the redu tion of rea tion s hemes by identi ation (by
hand or through sensibility analysis) of the limiting stages. The goal is the generation of
s hemes whi h an be used in pra ti al appli ations or in turbulent ows. The a urate
validation of these s hemes requires a omparison with the detailed ones. The automati
Detailed simulations des ribe as pre isely as possible the omplexity of the kineti
s hemes and transport phenomena. The ombustion of ommon arbohydrates in air
om-prises many hundreds of spe ies and some thousand elemental hemi al rea tions. The rst
stepistoidentifytheserea tionsandthe orrespondingrea tionrates. Theses hemes
( hem-i al me hanisms)are in orporated inthe simulationof rea tingows by means of hemi al
pre-pro essors. The rea tionrates introdu e numeri al stiness and highly non-linearityas
they followthe Arrheniuslaw, whi hin ludes anexponentialfa tor.
Although the speed and storage apa ity of modern omputers in reases ontinuously,
these detaileds hemesare notyetsuitableinmost asesforturbulentows be auseof their
omputational ost and the omplexity of modelling the turbulen e- hemistry intera tion.
This is the reason why these simulations are usually performed for laminar ows in simple
ongurations.
1.3. Literature overview
Multiple studies in the past few de ades have been presented on erning detailed
experi-mentaland numeri alanalysis of laminarames insimple ongurations. In parti ular, the
analysisof o-owlaminarameshasmotivatedagreatinterestduetotheirwideappli ation
inhouseholdandindustrialheatingsystems. Morere entlythesestudieshavebeenextended
topartiallypremixedames([62℄and[6℄)duetotheirpra ti alandfundamentalimportan e.
Be ause of their stability, partially premixed ames are used in Bunsen burners, furna es,
gas-turbine ombustorames,gas-reddomesti applian es,and other ommon ombustion
devi es. Re ent studies suggest that optimum operating onditions exist, whi h minimise
the pollutant emissionsand, thus, enhan e the design of leanerburning ombustors.
With in reases in omputationalpower, improvement of numeri al methods and use of
more a urate experimental te hniques, knowledge of the ombustion phenomenon taking
pla e in these ames has been onsiderably in reased.
Experimental studies have provided measurements of temperature, major spe ies,
rad-i als, nitrogen oxides and soot. Mass spe trometry, Raman and LIF te hniques have been
employed to study o-ow ames under dierent geometri al ongurations, equivalen e
ratios, and pressure- onditions ([62℄ and [85℄).
Con erning numeri al studies, from one of the rst multidimensionalsimulationsof
o-owmethane-airlaminarames arriedoutbyMit helletal[56℄,a onsiderableimprovement
of thea ura yofthe mathemati almodelsemployedforthe simulationshas beena hieved.
Detailed numeri alsimulationswith fully ellipti equations, omplex transportformulation
and detailed hemistry have been reported. C1 and C2 hemi al me hanisms are mainly
employed and ompared [44℄, mole ulartransport ismodelized under dierent assumptions
usually evaluated with simpliedmodels [7℄.
1.4. Codes used in this work
1.4.1. The FASTEST-3D ode
The numeri al simulations presented in this thesis have been performed with the ode
FASTEST-3D (Flow Analysis by Solving Transport Equation Simulating Turbulen e) [20℄,
a CFD tooldeveloped by the Institute forFluid Me hani s, University of Erlangenand the
Department of Numeri al Methods in Me hani al Engineering at Darmstadt University of
Te hnology. Thenumeri als hemeadopted inFASTESTtosolvethein ompressibleNavier
Stokes equations formulated in artesian oordinates is based on a pro edure des ribed by
Peri¢ [20℄, onsisting of a fully onservative se ond-order nite volume spa e dis retization
with a ollo ated arrangement of variables on stru tural, non-orthogonal, multiblo k grids.
A pressure orre tion methodof the SIMPLE algorithmwith Rhie and Chow[80℄
pressure-weighted interpolation for the iterative ouplingof velo ity and pressure is used, aswell as
an iterative ILU de omposition method by Stone for the solution of the sparse linear
sys-tems for velo ity omponents, pressure orre tion and temperature. All these features will
beexplained inthe following se tions.
1.4.2. The CHEMKIN-Pa kage
1.4.2.1. CHEMKIN (Kee, Rupley and Miller, 1989)
CHEMKIN [46℄is asoftware pa kage whose purpose isto fa ilitatethe formation,solution,
and interpretation of problems involvingelementary gas-phase hemi al kineti s. It
onsti-tutes an espe ially exible and powerful tool for in orporating omplex hemi al kineti s
intosimulationsof uiddynami s. Thepa kage onsistsof twomajorsoftware omponents:
anInterpreter andaGas-PhaseSubroutineLibrary. TheInterpreter isaprogramthatreads
a symboli des ription of an elementary, user-spe ied hemi al rea tion me hanism. One
output fromthe Interpreter isa data lethat formsalink tothe Gas-Phase Subroutine
Li-brary. This libraryis a olle tionofaboutone hundred highlymodular Fortransubroutines
that may be alled to return information on equation of state, thermodynami properties,
and hemi alprodu tionrates.
1.4.2.2. SENKIN (Lutz, Kee and Miller, 1988)
SENKIN [50℄ is a Fortran omputer program that al ulates the temporal evolution of a
elementary hemi al rea tions, and performs kineti sensitivity analysis with respe t to the
rea tion rates. The program onsiders veproblem types:
1. Adiabati system with onstantpressure
2. Adiabati system with onstantvolume
3. Adiabati system wherethe volume is aspe ied fun tion of time
4. System where the pressure and temperatureare onstant
5. System where the pressure is onstant and the temperature is a spe ied fun tion of
time.
The program uses the dierential equation system solver DASSAC ([10℄ and [11℄) to solve
boththe nonlinearordinarydierentialequationsthatdes ribethe temperatureand spe ies
massfra tionsandthesetoflineardierentialequationsthatdes ribetherst-order
sensitiv-ity oe ientsoftemperatureandspe ies ompositionwithrespe ttotheindividualrea tion
rates. The program runs in onjun tion with the CHEMKIN pa kage, whi h provides the
oe ientsand sour e terms for the equation system and serves as the user interfa e.
1.4.2.3. PSR (Glarborg et al., 1986)
PSR [32℄ is a Fortran omputer program that predi ts the steady-state temperature and
spe ies omposition in a perfe tly stirred rea tor (PSR). These rea tors are hara terized
by area torvolume, residen e timeor massow rate, heat lossortemperature, and the
in- omingtemperatureand mixing omposition. Themodela ountsfornite-rateelementary
hemi alrea tions. The governing equations are a system of nonlinear algebrai equations.
The program solves these equations using a hybrid Newton/time-integration method. In
ases where the Newton method has onvergen e di ulties, a time integration of the
re-latedtransientproblemhelpstobringthetrialsolutionintoNewton'sdomainof onvergen e.
The programruns in onjun tionwith the CHEMKIN pa kage, whi h handlesthe hemi al
rea tion me hanism.
Basi inputs totheSENKIN andthe PSR omputerprograms forthe asesunder study
are fuel omposition,temperature, residen etimeand pressure. ThePSR ongurations are
treated as a system where enthalpy and pressure remain onstant during the ombustion
pro ess. Sin e a set of algebrai equations is solved for the PSR, starting estimates for
the solution must be given. In luded in the PSR program is an option to use a modied
version of the STANJAN subroutine pa kage [78℄ to provide equilibrium ompositions as
initialsolutionestimates, ortouse previously al ulatedresultsasinitialsolutionestimates.
In this work we have onsidered an adiabati system with onstant pressure (problem
boundary, sothatthe totalmass of themixture is onstant. Inthe adiabati ase, sin e the
temperature is known, the energy equation is unne essary and the problem is ompletely
dened by the mass onservation equations. The SENKIN toolis able to treat one ase at
a time and all inputmust be introdu ed manually.
The SENKIN and PSR tools treat ideal ow models in ombination with hemi al
ki-neti s. The al ulation pro ess itselfdoesnot introdu e signi ant error sour es. However,
the assumptionof ideal owmodels, the hoi eof thermodynami and kineti data and the
fuel ompositionused, mayallinuen e thedis repan y between al ulated and
experimen-tal results. The use of ideal ow models is ne essary due to limitations in the pro essing
apa ity of today's omputers. Thermodynami and kineti data used are as up-to-date as
possible. The fuel omposition used is based on the examples found in the literature and
experimental onditions.
1.4.3. The FLUENT ode
FLUENT is one of the many ommer ial pa kages available for CFD. It is also the most
widelyusedgeneral-purposeCFDsoftwaretoperformuidowandheattransferanalysisof
realindustrialpro esses. Itusesthenite-volumemethodtosolvethegoverningequationsof
the ow. Itprovidesthe apabilitytousedierentphysi almodelssu hasin ompressibleor
ompressible,invis idorvis ous,laminarorturbulent,et . Supportedmeshtypesin lude2D
triangular/quadrilateral, 3D tetrahedral/hexahedral/pyramid/wedge, and mixed (hybrid)
meshes. Ofinterestinthe presentstudyisthe apabilityofFLUENT tosimulate hemi ally
rea ting ows under laminar onditions using a sti hemistry solver and a CHEMKIN
me hanisms asinput. The ombustionmodels availablein the ode in lude:
•
The generalized nite rate hemistry for N rea tions (forward/ba kward) with: ArrheniusmodelEddy-breakup (EBU) model
CombinedArrhenius/eddy-breakup model
Eddy dissipation on ept (EDC)
•
Conserved s alar•
Probability density fun tion (PDF) based formulation for diusion- ontrolled (non-premixed) rea tions (one ortwo mixturefra tions) using:Mixed-is-burned model
Chemi al equilibrium
•
A turbulent premixed ombustion model based on a turbulent ame speed losure model•
A partially premixed turbulent ombustion model•
Subgrid s ale ombustionmodels for large eddy simulations (LES),•
Laminar sti hemistry optionfor oupledsolver(used in the present work)•
Combustionsubmodels for oal, liquid,gas, and mixed fueltypes•
Pollutant formationmodels (NO
X
,Soot,...)•
Multi-step surfa e rea tions with multiple sites and site spe ies•
User-dened a ess to rea tionrates and sour e/sink terms•
Importof rea tionme hanismsin Chemkin format•
Several radiationmodelsChemi al me hanismsinCHEMKINformat anbereadinFLUENT andusedtodetermine
the hemi al sour e terms of the dierent spe ies rea ting in the ow. After reading the
me hanism and, eventually,the transportand thermodynami properties les in FLUENT,
the user must sele t the spe ies transport model and the volumetri rea tions option. The
6.2versionofFLUENThasbeenexpandedwithaverye ientlaminarsti hemistrysolver
whi h applies afra tional step algorithm. In the rst fra tional step, the hemistry inea h
ell is omputed for rea tion at onstant pressure for the ow time-step, using the ISAT
integrator. Inthe se ondfra tionalstep, the onve tion anddiusion termsare treatedjust
as in anon-rea ting simulation.
1.5. Content des ription
This thesis is divided into ve hapters. The rst of them is a brief introdu tion of the
work,thestateof theart andthetoolsinvolved. The se ond hapterdealswiththe physi al
and hemi al fundamentals. The basi ow equations for rea tive mixtures and transport
propertiesformulti- omponentmixtureswillbeintrodu ed,followed byabriefpresentation
ofsomegeneralaspe tsof hemi alrea tionsandnumeri almethods. Theoperator-splitting
te hnique is explained as well in this hapter. Chapter 3 shows the results of the
one-dimensional simulations for the CFD-solver and the hemi al kineti s pa kage for dierent
me hanisms and parameters like grid-spa ing,
Courant
number or temporal dis retization. Chapter 4 deals with two dimensional simulations for the simpler ase of onstant density.the ombustionpro ess. Thesimulationofone aseoflaminaramewithvariabledensityis
presented atthe endof this hapter. The veri ation ofthe resultshas been doneby means
of the CFD-Code FLUENT. In hapter 5, nally, a general dis ussion of the results and a
2.1. The Navier-Stokes equations
Tond outthe solutionofthe velo ityeldand for omputationofthe onve tiveand
diu-siveows,theNavier-Stokesequationsaresolved inFASTEST.TheNavier-Stokesequations
are a set of ve torial, nonlinear, partial dierential equations whi h, in the index notation
a ording to the Einstein summation onvention, present the following aspe t:
∂ρ
∂t
+
∂ρU
j
∂x
j
= 0
(2.1)∂(ρU
i
)
∂t
+
∂(ρU
i
U
j
)
∂x
j
= −
∂P
∂x
i
−
∂τ
ij
∂x
j
+ ρg
i
(2.2) where:τ
ij
= −µ
∂U
i
∂x
j
−
∂U
j
∂x
i
(2.3)is the stress tensor. The se ond term in the right hand side of equation 2.2 des ribes the
diusivetransportofmomentumdue toinnerfri tionandthe thirdterm orresponds tothe
gravity for e.
2.2. The energy equation
The equationthat providesthe temperatureeld isformulatedinFASTESTasanenthalpy
equation in the form:
∂(ρc
p
T )
∂t
+
∂(ρc
p
U
i
T )
∂x
i
= −
∂q
i
∂x
i
− τ
ij
∂U
i
∂x
j
(2.4)The indexes i and j take the value of the three spatial dire tions
i = 1, 2, 3
and of the omponentsof the velo ity ve torj = 1, 2, 3
respe tively.The losureof the onservationequations is ompletedthrough twostateequations, the
alori equation of state:
h =
N
s
X
i=1
Y
i
h
i
,
withh
i
= h
ref
i
+
Z
T
T
ref
c
pi
(T
′
)dT
′
(2.5)wherethe enthalpy isdenedasafun tionofthe temperatureT andspe ies massfra tions,
and the thermalequation of state, given by the ideal-gas-law:
p
k
= ρ
k
R
W
k
T
(2.6)where
T
isthe temperatureofthe mixture,R = 8.314J/(moleK)
istheperfe tgas onstant and whereρ
k
= ρY
k
,andW
k
are thedensityandthe atomi weightofspe ies k respe tively. For amixture ofN
perfe t gases, the total pressure is the sum of partial pressures:p =
N
X
k=1
p
k
(2.7)Sin e the density
ρ
of the mixture isρ =
P
N
k=1
ρ
k
equation2.6 an be written:p = ρ
R
W
T
(2.8)where W isthe meanmole ular weight of the mixture given by
1
W
=
N
X
k=1
Y
k
W
k
(2.9)Theapproximationofidealgas anbeusedinmost ombustionproblemsasthemixture
behaves likeanideal gas and the error introdu ed by this equation is negligible.
In equation 2.5 the referen e enthalpies
h
ref
i
are obtained from thermodynami tables. The enthalpy of the mixture an also be obtained from:h = h
ref
+
Z
T
T
ref
c
p
(T
′
)dT
′
(2.10) whereh
ref
is the enthalpy of the mixture atthe referen etemperature:
h
ref
=
K
X
k=1
Y
k
h
ref
k
(2.11)and
c
p
is the mean spe i heat of the mixture:c
p
=
K
X
k=1
2.3. The spe ies transport equations
The onservation of the hemi al spe ies is given by the transport equation for the mass
fra tion
Y
k
= ρ
k
/ρ
, whereρ
k
represents the density of the spe ies k:∂(ρY
k
)
∂t
+
∂(ρU
i
Y
k
)
∂x
i
= −
∂(ρV
ki
Y
k
)
∂x
i
+ ˙
ω
k
(2.13)V
ki
isthe i- omponentofthediusionvelo ityof spe iesk andω
˙
k
isthe hemi alsour e term, dened as the mass of spe ies k whi h is produ ed or onsumed per unit volume andtime. Be ause of the mass onservation it an bedemonstrated:
N
X
k=1
˙
ω
k
= 0
(2.14)and through the denition of mass fra tion:
N
X
k=1
ρ
k
= 1
(2.15)The diusion velo ities are obtained by solving the system:
∇X
k
=
N
X
j=1
X
k
X
j
D
kj
(V
j
− V
k
) + (Y
k
− X
k
)
∇p
p
+
ρ
p
N
X
j=1
Y
k
Y
j
(f
k
− f
j
)
forp = 1, N
(2.16)where
f
k
is the magnitude of the volumetri for e a ting on spe iesk
,D
kj
= D
jk
is the binary diusion oe ient of spe iesj
into spe iesk
and where the Soret ee t has been negle ted forthe sake of simpli ity.This omputationrepresents alinearsystem ofsize
N
2
whi hmust be solved inea h
di-re tion,ea hpointandinstantforunsteadyows. Thistaskisdi ultand omputationally
very ostly and, in most ases, Fi k'slawis used instead:
V
ki
Y
k
= −D
k
∂Y
k
∂x
i
(2.17)
Equation 2.17 oers a onvenient approximation for ombustionpro esses, where Lewis
numbers of individualspe ies vary in smallamounts in the ame front. The Lewis number
represents the ratio between the thermal diusion and the mole ular diusion of spe ies k.
This numberis ommonlyusedto hara terizethediusion oe ients. It an beexpressed
in the form:
Le
k
=
λ
ρC
p
D
k
=
D
th
D
k
(2.18)pointof theame toanother. From the kineti theory of gases [34℄we knowthat
λ
hanges roughly likeT
0
.7
,ρ
likeT
−1
andD
k
likeT
1
.7
sothat
Le
k
is hangingonly by afewper ents in aame.2.4. An introdu tion to hemi al kineti s
In a system of N spe ies rea ting through M rea tions in the form:
N
X
k=1
ν
′
kj
χ
k
⇋
N
X
k=1
ν
′′
kj
χ
k
forj = 1, M
(2.19)where
χ
k
represents the symbol andν
′
kj
, ν
kj
′′
are the molar stoi hiometri oe ients as rea tant and produ t respe tively of spe ies k in the j rea tion, the amount of spe ies jprodu ed or onsumed perunit time and volume isthen:
˙
ω
k
= W
k
M
X
j=1
(ν
′′
jk
− ν
jk
′
)r
j
(2.20)where
r
j
representstherea tionrateofthe j-threa tion. Thephenomenologi allawof mass a tion statesthatthe rea tionrateisproportionaltothe produ tofthe on entrations. Foranequilibriumrea tionlike2.19, the net rea tionrate isthe dieren ebetween theforward
and the reverse rea tion rates and an be expressed inthe form:
r = k
f
N
Y
k=1
[χ
k
]
ν
′
k
− k
r
N
Y
k=1
[χ
k
]
v
′′
k
(2.21)where
[χ
k
]
represent the molar on entration of the spe ies involved inthe rea tion.Theforwardrate onstantforthej-threa tionisgenerallyassumedtohavethefollowing
Arrhenius temperature dependen e:
k
f
j
= A
j
T
β
j
exp(
−E
j
RT
)
(2.22)In this equation
A
j
,β
j
andE
j
represent the pre-exponential fa tor, the temperature exponent and the a tivation energy respe tively. These values are hara teristi for ea hrea tion and do not depend on the temperature. The reverse rea tionrate isrelated to the
forward rea tionrate through the equilibrium onstant by:
k
r
=
k
f
K
eq
The equilibrium onstantfor the rea tion j an be obtained through the relationship:
K
eq
j
= exp
∆S
0
j
R
−
∆H
0
j
RT
p
atm
RT
P
N
k=1
ν
kj
(2.24)The use of equilibrium onstants for rea tions involvingele trons isnot appropriate. In
the ase of ombustion rea tions this approximation is valid and will be used throughout
this work.
2.4.1. Chemi al Me hanisms
Mathemati ally,a hemi alme hanismisaset of oupledandoftensti,rst-order
dieren-tial equations. There are many software pa kages available that e iently and simplysolve
these equationstoobtainspe ies on entrationsasafun tion oftime. Su hsoftware an be
applied to a wide range of omplex hemi al systems su h as multi-phase CVD-rea tions,
ombustion, atalysis and many other appli ations. A me hanism in ludes a list of all
primary, se ondary, and intermediate rea tions whi h give ertain, essentially qualitative,
information about the fate of aspe ies.
In ombustion systems, kineti models have thousands of elementary rea tions and a
large number of rea tiveintermediates. Forexample there are 3662 rea tions involving 470
hemi alspe ies onsidered in the simulations of n-hexane ombustion by Glaudeet al [26℄
and 479206 rea tions and 19052 hemi al spe ies in simulation of tetra-de ane ombustion
performed by De Witt et al [18℄. Gri-Me h is a ompilation of 325 elementary hemi al
rea tions and asso iated rate oe ientexpressions and thermo hemi alparametersfor the
53 spe ies involved in them. Su h me hanisms likethe ones mentioned above are too
om-putationally expensive and, in most ases, annot be used in the simulation of a full s ale
ombustion hamber. Manyredu tionte hniqueshavebeendevelopedinthelastyears,that
allow the generatation of simple me hanisms from the detailed ones without losing riti al
information about the main features of the hemi al pro ess. Some of the most ommon
redu tion te hniques an be found below.
The hemi al me hanisms used to simulate methane and hydrogen ombustion in the
present work are the ones from Kee et al. [46℄ for hydrogen and Ern and Smooke [24℄ for
methane ombustion. The spe ies involved in these me hanisms, as well as the hemi al
rea tions with their orrespondingArrhenius oe ients an be seen inAppendix A.
2.4.2. Me hanism redu tion methods
2.4.2.1. Equilibrium Chemistry
A hemi al rea tion is in equilibrium when the spe ies on entrations remain onstant in
en-ergy or through integration for
t → inf inity
of the following dierential equations for a homogeneous time-dependent system:dY
k
dt
= W
k
, k = 1, ..., N
whereW
k
= ˙ω
k
/ρ
(2.25) Forlaminar amesthe equilibriumhypothesisis inexa t inmost asesbe auseinterme-diate spe ies annot be determined and the spe ies on entrations are only valid very far
away from the ame front. The method for me hanism redu tion through partial
equilib-rium is based on the assumption that the fastest rea tions are in equilibrium. This is only
true whentherea tionratesforthe forward andba kward rea tionsare very lose. One an
solvethese elementaryrea tions through algebrai relationshipsand the omputationof the
Ja obi matrix an be avoided. The justi ation of the lassi ation in fast and slow s ales
takes pla e through omparison with ow time s ales. This means that an analysis of ea h
rea tion's Damköhler number must be done. Some studies have shown that the strategy
of the partialequilibrium is limitedto high-temperature, mixing ontrolled diusion ames
involving rapidly rea ting omponents.
2.4.2.2. Quasi Steady State Assumption
For explanation of this methodlet's onsider the following rea tion:
A → B → C
(2.26)The evolution ofthe on entration ratesfor spe iesA, B and C an bedes ribed by the
followingdierentialequations:
d[A]
dt
= −k
12
[A],
d[B]
dt
= k
12
[A] − k
23
[B],
d[C]
dt
= k
23
[B]
(2.27) The solution of the rst equation an be found easily:[A] = [A]
0
exp(−k
12
t)
(2.28) If the rea tion velo ities have dierent orders of magnitude, for examplek
12
≪ k
23
, the on entration of spe ies B in the mixture will be very small. The velo -ity at whi h B is onsumed is almost as high asthe generation velo ity and therefore thereis anequilibrium:
d[B]
dt
= k
12
[A] − k
23
[B].
(2.29) This is the quasi-steadiness prin iple (see [98℄), a ording to this assumption theof spe ies Cwe obtain the followingexpression:
d[C]
dt
= k
23
[B]
(2.30)By using the quasi-steadiness assumption, the on entration of C an be expressed in
terms of the on entrationof A:
d[C]
dt
= k
12
[A] = k
12
[A]
0
exp(−k
12
t)
(2.31) Integrating this expression one obtains:[C] = [A]
0
(1 − exp(−k
12
t))
(2.32) The quasi-steadiness assumption has the advantage of de oupling the dierentialequa-tions 2.27, whi h redu es the stiness of the Ja obi matrix and, this way, the omplexity of
the omputation. The spe ies havingshort periodsof existen e are not eliminatedfrom the
me hanism but an beevaluatedthrough simple algebrai expressions.
2.4.2.3. ILDM-Model
TheIntrinsi Low-DimensionalManifoldmethodintrodu edbyMassandPope[51℄identies
the fastpro essesbyusinganeigenvalueanalysisofthelo alJa obianofthe hemi alsour e
terms. Byomittingthe onve tion anddiusionterms inthe spe iesequation weobtainthe
time-dependentdierentialequation system 2.25.
Writingtheequationinve tornotationoneobtains:
d
Y/dt =
W,withY= (Y
1
, Y
2
, ..., Y
N
)
T
and W
= (W
1
, W
2
, ..., W
N
)
T
. This ve tor notationis used to des ribe the mixture as a
N
-dimensional spa e alled the omposition spa e. Formallyp, and h are needed to des ribethe omplete omposition ofthe mixturebut, sin ethey are onstantinthis ase,they have
not beenintrodu edinthisve tornotation. Toidentifythefastandslow hemi alpro esses,
the hemi alsour e term W is linearized aroundthe referen e ompositionY 0 :
d
Ydt
≈ W (
Y 0) + J(
Y 0)(
Y−
Y 0)
(2.33) whereJ(
Y 0)
istheN ×N
Ja obianmatrixwithelementsJ
ij
= ∂W
j
/∂Y
i
|
Y
0
. Thelo al
har-a teristi s ofthe system an beexaminedbytransforming2.33 intothebasisof eigenve tors
of the Ja obianmatrix. The Ja obianmatrix istherefore diagonalizedas follows:
J
=
SLS−1
(2.34)
where L is adiagonalmatrix withthe eigenvalues
λ
k
. The olumnsof the matrix Sare the right eigenve torssK
ofthe ja obianmatrix. Byusing the transformationY
=
Sˆ
2.33 an be writteninthe basis of eigenve tors:
d ˆ
Ydt
= ˆ
W0
+
L( ˆ
Y− ˆ
Y 0)
(2.35) withˆ
W 0=
S−1
W(
Y 0)
. Asaresult ofthis transformation,thedierentialequationsin2.25 are de oupled and the evolution of ea h modeY
ˆ
k
is des ribed by:d ˆ
Y
k
dt
= ˆ
W
0
K
+ λ
K
( ˆ
Y
K
− ˆ
Y
K
0
).
(2.36)This equation gives us the basis for a time-s aleanalysis of the dierent modes. When
the absolutevalue of the eigenvalue
λ
K
is small, the typi altime s ale of the orresponding mode is given byˆ
(W
0
K
)
−1
. On the other hand, if the absolute value of the real part of
the eigenvalue is large, the time s ale is given by
λ
−1
K
. If the magnitude ofλ
K
is large, movements in the dire tion of the asso iated eigenve tor will pro eed fast. Modes with apositive real part of the eigenvalue willgrow exponentiallyin time. For negativereal parts
the orrespondingpro esses willrelaxtowards asteadystate. Modes with
λ = 0
orrespond to onserved quantities su h aselement mass fra tions.It an be on luded that the introdu tionof steady-state equationsis most suitable for
modes orresponding toeigenvalueswith largenegativereal parts. Ifthe modes areordered
in su ha way thatthe eigenvalueswith the lowest index orrespond tothe fastest damping
pro esses, the steady-state equationsmay bewritten as:
s
L
k
W= 0, k = 1, ..., N
st
(2.37) where sL
K
are the left eigenve tors of the Ja obian matrix. Sin e the analysis is based on
the lo alJa obianmatrix,the ombinationofspe ies insteady state hangesin omposition
spa e. The olle tionof all points in ompositionspa e satisfying2.37 forms an
(N − N
st
)
-dimensionalsubspa e: theintrinsi low-dimensionalmanifold. Intheredu edmodel,thefasthemi alpro esses areassumed insteadystate andonlymovementswithinthe manifoldare
allowed. Conservation equations have tobe solved for these slowly hanging variables only,
whi h redu es the omputational ost.
2.5. Combustion Theory
The basi on epts regarding hydro arbon ombustion will be summarized here. We will
restri t ourselves to methane and hydrogen ombustion, sin e these are the fuels that take
part in the numeri al simulationspresent inthis thesis.
Air is basi ally a mixture of nitrogen (
N
2
) and oxygen (O
2
). Any other omponents are negle ted inthis work (Argon,CO
2
,...) be ausethey are present in very small amountsand do not play a relevant role in methane or hydrogen ombustion. Let
β
be the ratio between the number of moles of nitrogen and oxygen. The value 3.764 has been used forthis parameter inthe present work.
Methane ombustion in presen e of air an be roughly des ribed by one rea tion with
the following balan eof produ ts and rea tants:
CH
4
+ 2(O
2
+ βN
2
) → CO
2
+ 2H
2
O + 2βN
2
(2.38) In the ase of hydrogen ombustion,the balan eis as follows:H
2
+
1
2
(O
2
+ βN
2
) → H
2
O +
1
2
βN
2
(2.39)In this simplemodelnitrogendoesnot rea tand itsonlyrole isthat ofasolventfor the
otherspe ies. Methaneandoxygenaretransformedin arbondioxideandwatervaporwhile
hydrogen ombustionleadstothe generationofwatervaporastheonlyprodu t. Thismodel
onstitutes a very rough approximation of what happens in real ombustion and won't be
used inlater omputations.
2.5.1. Nitrogen rea tions
A tually,thenitrogenpresentintheairdoesnotremainuntransformed duringthe
ombus-tionpro ess. Infa t,apartofthenitrogenis onvertedintonitrogenoxides. Theseprodu ts
are pollutantsandtheir emissionsmust be ontrolledfollowingaverystri tregulation. The
onsideration of the rea tions involvingnitrogen isthus oftenrequired.
A very ommon pro edure onsists of de oupling the simulation of the ombustion and
thepredi tionofthenitrogenoxides. Followingthisapproa h,theameissimulatedwithout
onsidering the hemistryof the nitrogen. After this, when allother spe ies are determined
in the ame, the rea tions involving nitrogen are reprodu ed. This pro edure is only an
approximation,but it isjustied by the very long hara teristi times of nitrogen rea tions
in omparison with other hemi alrea tions taking pla e inthe ombustionpro ess.
In the following study we willmake use of the assumption that nitrogen does not rea t
during the ombustion pro ess.
2.5.2. Ex ess air and air fa tor
One kilogram of fuel requires a ertain minimum of ambient airto be fully ombusted. We
all this minimum amount of air the stoi hiometri air or theoreti al air to ombust the
fuel. Thestoi hiometri airwill ompletely ombustthefuelto arbondioxide(
CO
2
),water (H
2
O
) and sulfur dioxide (SO
2
), if sulfur is present. If the fuel does not get enoughair for ombustionitwillgeneratesmokeandapotentiallyunhealthymixtureofsta kgasprodu ts.Inaddition,energyiswasted. Thesameappliesiftoomu hex essairisusedfor ombustion.
A less trivialissue in ombustionte hnology istherefore toensurethe properamount ofair
that minimizesenvironmentalimpa t and fuel onsumption.
For onvenien e we dene the stoi hiometri air as the air to fuel ratio, AF (kg air/kg
fuel), and the ex ess airfa tor as:
λ =
Mass of air (Kg) to combust one Kg of f uel
Stoichiometric air (AF )
(2.40)λ
values greaterthan 1.0indi ateex ess airand are alledlean mixtures.λ
values less than 1.0 indi ateex ess fuel for omplete ombustion,and are alledri h mixtures.The airtofuel ratio(AF)is apropertyof afuel that an be al ulatedfrom its
ompo-sition. Table 2.1shows theAF ratio and maximumwet
CO
2
orrespondingtosome fuelsof general interest.Table 2.1.: Air toFuelratio for variousFuels
Fuel Phase AF
CO
2
max
wet
Very lightfuel oil liquid 14.27 13.56Light fueloil liquid 14.06 13.72
Medium heavy fueloil liquid 13.79 14.00
Heavy fuel oil liquid 13.46 14.14
Bunker C liquid 12.63 16.23
Generi Biomass(maf) solid 5.88 17.91
Coal A solid 6.97 16.09
LPG (90 P : 10B) gas 15.55 11.65
Carbonsolid solid 11.44 21.00
TheAF ratiohasnothingtodowiththefurna edesignor ombustionpro ess,while
λ
is aparameterthattellsushowe ientlyafuelwas ombusted. The loserλ
istoone,themore e ient is the furna eor burnerdesign andoperation. Operatingvery lose tothe minimalamount of air (= stoi hiometri air) has the inherent danger of smoke, CO generation and
high temperatures leading tothe formation of thermal
NO
X
(Zeldovi h-me hanism[33℄).2.5.3. Low Ma h number ombustion
The lowMa hnumberapproa h hasbeenused inthisstudy. More detailedinformation an
be found in [77℄. The approa h is based on the fa t that, for low Ma h numbers, pressure
vari-ations are situated many orders of magnitude below the atmospheri pressure (the burner
is supposed to be in thermodynami equilibrium with the surrounding atmosphere).
Con-sidering this, spe i equations an be established similar to those used for in ompressible
ows but allowing variationsin the density whi h are essentialfor ombustion.
The pressure an bede omposed inthesummationof twoterms, thesurrounding
atmo-spheri pressure, whi h is relevant for the thermodynami state of the uid and a variable
hydrodynami pressure. The rst term is onstant while the se ond is a fun tion of time
and spa e:
p(~x, t) = p
atm
+ ˜
p(~x, t), ˜
p(~x, t) ≪ p
atm
(2.41) When regarding the ow pressurep
, one an assume that itisequal tothe atmospheri pressure by negle ting the hydrodynami omponent. If we are interested in the pressureu tuations, it is the hydrodynami pressure that has to be taken into a ount sin e
p
atm
remains onstant intime and spa e.Forall al ulationsperformedinthepresentworkandpresentedinthefollowing hapters,
the surroundingatmospheri pressurehas been onsideredequaltotheatmospheri pressure
(
101325 P a
).2.6. Numeri al Methods
The Navier-Stokesequations annotbesolvedanalyti allyex eptforafewsimpleowtypes
under ertain assumptions. The system of partial dierential equationsmust be dis retized
andsolvedthroughiterativemethods. Inthisse tionsomeofthenumeri almethodsusedfor
theresolutionofthisequationssystemareenumeratedandexplained. Someofthesemethods
were alreadyavailableintheCFD-Code FASTEST-3D andsome havebeen implementedas
a part of the present work.
2.6.1. The nite-volume method
Let us onsider the generi onservation equationfor a quantity
φ
:Z
S
ρφv · ndS =
Z
S
Γgradφ · ndS +
Z
Ω
q
φ
dΩ
(2.42)and assumethatthe velo ityeld andalluidpropertiesare known. Thedomainisdivided
in a nite number of small ontrol volumes. The onservation equation 2.42 is applied to
ea h ontrol volume as well as to the solution domain as a whole. If we sum equations for
all ontrolvolumes we obtain the global onservation equation (surfa e integralsover inner
2.6.1.1. Surfa e integrals
The surfa eof the ontrolvolume anbede omposedinfour(2D)orsix (3D)fa esdenoted
by e, w, n, s, t and b orresponding to their dire tion. The ux through the boundary of
our ontrol volume is:
Z
S
f dS =
X
k
f dS
(2.43)where f is the omponent of the onve tive
(ρφv · n)
or diusive(Γgradφ·n)
ve tor in the dire tion normaltothe fa e.To al ulate the surfa e integral two levels of approximation are used. The integral is
approximated interms of the variable values at one or more lo ations onthe ellfa e orin
terms of the values at the enter of the ontrol volumes. If the integral is approximated as
a produ t of the integrand at the fa e enter and the fa e area we obtain a se ond-order
approximation. The mean value of the ux through the
e
fa ef
e
is then al ulated by interpolation ofthe valuesof f atthe adja ent nodes. This an bedone by substituting theintegral:
Z
S
e
f dS = f
e
S
e
(2.44)Other higher order approximations an be a hieved by onsidering the values of f at
more lo ationsonthe fa ee.
The approximations to the integrals require the values of variables at lo ations other
than the omputationalnodes. The integranddenoted by
f
, involves the produ tof several variables and/or variable gradients at those lo ations:f = ρφv · n
for the onve tive ux andf = Γgradφ · n
forthediusiveux. Theinterpolationte hniquesused toapproximate the value ofφ
and its derivativeare:•
Upwind Interpolation: the value ofφ
is approximated by it is upstream value:φ
e
=
φ
P
if(v · n)
e
> 0
φ
E
if(v · n)
e
< 0
(2.45)•
CentralDieren eS heme: the valueφ
e
an beapproximatedby the linearexpressionφ
e
= φ
E
λ
e
+ φ
P
(1 − λ
e
)
(2.46)where
λ
e
=
x
e
−x
P
x
E
−x
P
.
Using the Taylor series expansion of
φ
E
about the pointx
P
the rst derivative dis-appears from the equation forφ
e
and the error is proportional to∂
2
φ/∂x
2
, this is,
andEoersaverysimpleexpression forthe gradient,neededforevaluationofdiusive uxes:
∂φ
∂x
≈
φ
E
− φ
P
x
E
− x
P
(2.47) 2.6.1.2. Volume integralsVolumeintegralsare approximated bythe produ t ofthe ellvolumeand the meanvalue of
f inthe ell:
Q
P
=
Z
Ω
qdΩ = q∆Ω ≈ q
P
∆Ω
(2.48)where
q
p
is the value of q atthe enter of the ontrol volume. This is a rst-order approx-imation, the solution is exa t if the variation of q is linear in spa e. An approximation ofhigher order requires values of q atmore lo ations inthe ell.
2.6.1.3. Deferred orre tion
Highorderuxapproximations anbe al ulatedexpli itlybyusingvaluesfromtheprevious
iteration. This approximation an be ombinedwith an impli itlower-order approximation
whi h uses onlyvalues atnearest neighbors:
F
e
= F
e
L
+ (F
e
H
− F
e
L
)
old
(2.49)The term in bra kets may bemultipliedby a fa tor
β
, thusblending the two s hemes. A high order approximation provides a more a urate solution when the grid is neenough to apture the essential details of the solution.
2.6.2. The SIMPLE algorithm
The SIMPLE algorithm for the velo ity-pressure oupling has been used in this work. It
wasdeveloped by Patankar and Spalding [66℄ and has sin e then been rened by a number
of authors.
Variantsrejoi ing in the names of SIMPLEC [94℄, [79℄, SIMPLEX [79℄, SIMPLEN [92℄,
SIMPLER [66℄ and PISO [39℄ aim to improve the ouplingof the momentum and pressure
equations via minor modi ationsof the SIMPLE algorithm.
Thes hemeisapredi tor- orre tormethod,withaninitialestimateforthevelo ityeld
from the Navier-Stokes equations being orre ted with the ontinuity equation to for e the
onservation of mass. The predi tion and orre tion operationsare en losed in an iterative
The initials heme by Patankar and Spaldingwasfor a staggered Cartesian mesh, with
the velo ity values being lo ated at the fa es of nite volume ells, and the pressure,
tem-perature and other s alar variables being lo ated at the ell enters. Rhie and Chow [80℄
extended the method to use ollo ated grids, where the velo ities and the other variables
are all lo ated at the ell enters, and this has been further developed by Peri¢ and other
authors ([71℄, [28℄). Su h a grid allows an easier onversion tonon-Cartesian meshes. Here
it willbe des ribed forCartesian meshes.
The rst stage of the al ulation pro ess is the resolution of the dis retized versions
of the momentum equations 2.2 using the urrent estimate of the pressure eld, and using
a ell fa e mass ux that is interpolated from the urrent estimate of the velo ity eld
(this interpolation pro edure is dis ussed in more detail in Se tion 2.6.4). The momentum
equations 2.2 are in the same general form as the generi transport equation. For a given
mass uxeld and pressure eld they an bedis retized intoequationsof the form:
a
P
u
∗
P
+
X
n=nb
a
n
u
∗
n
= S
x
+ A
x
dp
dx
a
P
v
P
∗
+
X
n=nb
a
n
v
n
∗
= S
y
+ A
y
dp
dy
(2.50)a
P
w
∗
P
+
X
n=nb
a
n
w
∗
n
= S
z
+ A
z
dp
dz
whereu
∗
p
,v
∗
p
andw
∗
p
are the new estimates of velo ity in the x, y and z. axis,and nb refers to the neighboring ells.A
x
, A
y
andA
z
represent the areas of the ell fa es normal to thex, y
andz
axis. The pressure gradient an be found by interpolating the pressure eld at the ell fa es using a linear interpolation, and then approximating the gradient a ross theell with a entered dieren e as:
dp
dx
≈
p
e
− p
w
∆x
,
dp
dy
≈
p
n
− p
s
∆y
,
(2.51)dp
dz
≈
p
t
− p
b
∆z
,
for a regularmesh where
∆x, ∆y
and∆z
are the elldimensions.After the al ulationof the velo ity eld estimates, the ellfa evelo ities an be
inter-polatedfromtheir values atthe ell enters, and the ellfa emass uxes anbe al ulated.
Forthe easternfa eof a ellthe velo ity normaltothe fa eis
u
e
,whilstthe fa ehasanareaA
e
. The mass ow a ross the fa eis:In generalthis interpolatedvelo ity eld willnot bemass onserving (i.e.,itwillnot havea
dis rete divergen e of zero), and so willnot satisfy the dis retized version of the ontinuity
equation:
m
e
− m
w
+ m
n
− m
s
+ m
t
− m
b
= 0,
(2.53) whi h an be writtenfor the fa e velo ities ona Cartesian meshesas:ρA
e
u
e
− ρA
w
u
w
+ ρA
n
v
n
− ρA
s
v
s
+ ρA
t
w
t
− ρA
b
w
b
= 0,
(2.54)Wethereforewishto al ulatea orre ted velo ityeld
u
∗∗
,
v
∗∗
and
w
∗∗
that ismass
onserv-ing, together with a orresponding pressure eld
p
∗∗
. We do so by adding a velo ity and
pressure orre tion tothe originalestimation of the velo ity and pressure elds:
u
∗∗
= u
∗
+ u
′
,
v
∗∗
= v
∗
+ v
′
,
(2.55)w
∗∗
= w
∗
+ w
′
,
p
∗∗
= p + p
′
,
where a dash′
signiesthe orre tion eld.
The expressions inequation 2.55 are substituted into the
u
equation inequation 2.50a
P
(u
∗
P
+ u
′
P
) +
X
n=nb
a
n
(u
∗
n
+ u
′
n
) = S
x
+ A
x
d
d
x
(p + p
′
),
(2.56)and the sum of the neighboring velo ity terms approximated by:
X
n=nb
a
n
(u
∗
n
+ u
′
n
) ≈ A
x
dp
′
dx
(2.57)whi h should be validas
p
′
→ 0
and
u
′
→ 0
. Subtra ting the momentum equationgives an
expression relatingthe orre tion pressure and velo ity eld toea h other,
a
P
u
′
P
≈ A
x
dp
′
dx
,
(2.58) oru
′
P
=
A
x
a
P
dp
′
dx
,
v
′
P
=
A
y
a
P
dp
′
dy
,
(2.59)w
′
P
=
A
z
a
P
dp
′
dz
,
where similar approximations have been made for the
x, y
andz
omponents of velo ity. By interpolating the expressions in equation 2.59 to the fa es of the ell, the orre ted ellfa e velo ities normalto the fa eare given by:
u
′
e
=
A
xe
a
P
e
p
′
E
− p
′
P
δx
e
,
v
′
n
=
A
yn
a
P
n
p
′
N
− p
′
P
δy
n
,
(2.60)w
′
t
=
A
zt
a
P
t
p
′
T
− p
′
P
δz
n
,
with the
a
P
terms being approximated atthe fa es by a linear interpolationa
P
e
=
a
P
P
+ a
P
E
2
,
a
P
n
=
a
P
P
+ a
P
N
2
,
(2.61)a
P
t
=
a
P
P
+ a
P
T
2
,
In this interpolationa
P
P
is thea
P
termin the equation for the ellP
, whilsta
P
E
is thea
P
term in the equation for ellE
. Substituting the equations in 2.55 into the dis retized ontinuity equation 2.54 yieldsA
e
(u
∗
e
− u
′
e
) − A
w
(u
w
∗
+ u
′
w
) + A
n
(u
∗
n
+ u
′
n
)
−A
s
(u
∗
s
+ u
′
s
) + A
t
(u
t
∗
+ u
′
t
) − A
b
(u
∗
b
+ u
′
b
) = 0
(2.62)
Usingthe expressions for
u
′
fromequation2.60and fa torizingyieldsfollowingequation
for the pressure orre tion:
b
P
p
′
P
+ b
E
p
E
′
+ b
W
p
′
W
+ b
N
p
′
N
+ b
S
p
′
S
+ b
T
p
′
T
+ b
B
p
′
B
= c
(2.63) whereb
E
=
A
2
e
a
Pe
, b
W
=
A
2
w
a
Pw
, b
N
=
A
2
n
a
Pn
, b
S
=
A
2
s
a
Ps
, b
T
=
A
2
t
a
Pt
, b
B
=
A
2
b
a
Pb
b
P
= −(b
E
+ b
W
+ b
N
+ b
S
+ b
T
+ b
B
)
c =
1
ρ
(m
w
− m
e
+ m
n
− m
s
+ m
t
− m
b
)
This an be solved for the pressure orre tion