2SteadyOneDimensionalDetonations35 D media at restmedia at restdownstreamsonic planeshock frontexothermicreaction 30 150 50 p115 150 25 p1p1 translationalrotational equilibrium 10 20 150 ID: 254139
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Springer-VerlagBerlinHeidelberg2012 2SteadyOne-DimensionalDetonations35 D media at restmedia at rest(downstreamsonic planeshock frontexothermicreaction 30 50 p115 25 p1p1 translational/rotational equilibrium (10 20 60GPa10 40GPa vibrational redistribution/bond breaking (10 0GPa sonic plane sonic plane unsteady expansion shock front shock front pressurepressure Fig.2.1.SchematicoftheZNDstructureofadetonationwave,forbothgaseousdetonationatatmosphericconditionsandcondensedphasedetonation,etc.)occursaswellasslowercondensationanddiusion-controlledpro-cessessuchascarbonparticulateformation.AcurrentpictureoftheNon-EquilibriumZND(NEZND)structureofcondensedphasedetonationwaveshasbeenpresentedbyTarver[]andinChap.ofthisvolume.Thispictureisfurthercomplicatedbythefactthatallknowngaseousdetonationsarehydrodynamicallyunstable(Chap.ofthisvolume)andthisinstabilityismanifestedasatransient,three-dimensionalcellularstructure(seeChaps.inthisvolume).Condensed-phaseexplosivesaresimilarlycomplex.Mostliquidexplosivesdisplayastructureoftransversewavesthatarebelievedtobesimilartothoseingaseousdetonation,onlyonamuchnerscale.Solidexplosivesasusedinmostapplicationsarepolycrystalline, 40A.Higginsbetweenand),thelocationofthemaximumreactionrate,ortheinectionpointofthetemperatureprole.Asactivationenergyisincreasedfrom =10to =25,thereactionzoneincreasesbyanorderofmagnitudeinlength.Increasingfrom =25to =50resultsinanadditionaltwoordersofmagnitudeincreaseinreactionzonelength.Thelengthscaleofthesereactionzonesissomewhatarbitrary,duetotakingthevalueofasunity.Whatismoresignicantistheincreas-sharpnessofthereactionproleasactivationenergyisincreased.Aloweractivationenergyresultsinarelativelygradualincreaseintemperaturebegin-ningimmediatelyaftertheshock,whilethehighactivationenergyresultsinalongplateauofnearlyconstantconditionsfollowedbyacomparativelyrapidenergyrelease.Thisfeatureofhighactivationenergyreectstheunderly-ingtemperaturesensitivityofchemicalreactionsthatmustbeactivatedandisoneofthemostsignicantandreoccurringthemesinthedevelopmentofdetonationtheory.ThetemperatureprolesinFig.2.2featuremaximathatoccurbeforetheendofthereactionzone;thisismostclearlyvisibleinthetemperatureproleforthe =50caseduetothesteepnessoftheprolebutitispresentinallcasesplotted.Beyondthismaximum,exothermicheatreleaseintheowhastheeectofloweringthetemperature.Thiscounterintuitiveresultisaconsequenceoftheheatreleaseresultingingreaterowaccelerationandpres-sure/densityreductionthanitscontributiontoraisingthestatictemperatureoftheow.ThistemperaturedecreasewithheatadditionoccurswhentheMachnumberisintherange 1;thisresultiswellestablishedincompressibleone-dimensionalowwithheataddition(Rayleighow).Itisinterestingtoexplorewhathappensifacalculationofthereactionzonestructureisinitializedwithanon-CJdetonationvelocity.ThisisdoneinFig.2.3for =25,wherethesolutionwasinitializedwiththepost-shockstateforshockMachnumbers20%greaterand20%lessthantheCJMachnumber.Forthestrongershockcase,thereactionzonestructurecanbesolvedfor,andasthereactionprogressvariablereaches=1,theowisseentoremainsubsonic.Thissolutioncorrespondstoastrongdetonation,i.e.,thebranchoftheproductHugoniotcurveabovetheCJdetonationpointonthe(p,v)plane.Thiscaseisalsoreferredtoasanoverdrivendetonation,sincethedetonationisbeingforcedtopropagateataspeedgreaterthantheCJspeed,andtheheatreleaseisinsucienttochoketheow.Ifthesolu-tionisinitializedwithasub-CJdetonationvelocity,thenumericalintegrationencountersasingularityastheowbecomessonicwhilethereactionrateisstillnite(1)in(2.16).Inthiscase,theheatreleaseissucienttochoketheowbeforeaddingthefullheatrelease,andfurtherheatadditiontoasonicowisnotpermittedinasteadysolution.ThissingularitywillappearforanyinitialconditionthatiseveninnitesimallylessthantheCJspeed.Asimilarresultisobtainedifthewavespeedisxedandtheheatreleaseincreasedincrementally.Theappearanceofamathematicalsingularitymay 2SteadyOne-DimensionalDetonations41 X Mach number M0.20.30.40.50.70.80.91.01.1 singularityX singularity 80% 120% X -0.50.00.51.0 singularity X Distance xp/p1102103104105Distance x102103104105Distance x102103104105Distance x1021031041051020304050607080 singularity Fig.2.3.StructureofZNDdetonationforreactionzonestructureinitializedwithaCJdetonation,adetonationoverdrivenat120%,andashockat80%showingpressure,temperature,reactionprogressvariable,andowMachnumber =25,=10,2.Thesub-CJshockdoesnotcorrespondtoasolutionofconservationlaws,resultinginasingularityappearinginthenumericalintegrationappearalarming,butrecallthattheCJdetonationistheminimumvelocitywaveconsistentwiththegoverningconservationlaws.Thefactthatasin-gularityisencounteredinnumericallyintegratingthroughthereactionzoneinitializedwithaspeedlessthantheminimumspeedsimplyreectsthatanattemptisbeingmadetosolveaowusinginitialconditionsforwhichnosteadysolutionexists.2.3PathologicalDetonationsInsteadoftheonestepreactionAB,consideratwo-stepreactionwithAreactingtoformB,whichinturnreactstoformCReaction1:AB(2.19)Reaction2:BC(2.20) 2SteadyOne-DimensionalDetonations43numberbasedontheequilibriumheatreleaseisequil781.Initial-izingtheintegrationof(2.23)withthevonNeumannstatebasedonthisshockMachnumberresultsinasingularitybeingencountered,asshowninFig.2.4.ItisnecessarytoincreasetheshockMachnumbertoeigen(orapproximately6%greaterthantheCJspeedbasedonequilibrium)inordertondasolutionthatdoesnotencounterasingularitywithinthereac-tionzonestructure.Thisvaluecanonlybefoundbytrialanderrorintegrationofthegoverningordinarydierentialequations.ThetermChapman Jouguetisstillusedtorefertothissolution,sinceitfeaturesasonicsurfaceconsistentwithJouguetsoriginalcriterion.Todierentiatethesetwocases,theywillbereferredtoastheCJequilibriumsolutionandtheCJeigenvaluesolution.Finally,toeliminateanyconfusionastowhythepresenceofanendother-micreactionresultsinagreaterthanequilibriumdetonationvelocity,notethatthedetonationvelocityassociatedwiththerststageexothermicreac-tionalonewouldbe)=9486.Theendothermicreactionreducestheeectiveheatreleaseanddetonationvelocityincomparisontothisvalue,butthepathologicalbehaviorresultsinadetonationvelocitythatisgreaterthantheCJequilibriumsolutionbasedonthetotalheatrelease.Numericalintegrationofordinarydierentialequationswithapotentialsingularityembeddedwithinthesolutionisanotoriouslydicultproblem.Itmaybenecessarytointerveneinthenumericalalgorithmusedinordertoselectasolution,sinceuponencounteringthesonicpoint,thedierentialequationsbecomeindeterminate.Alternatively,itispossibletostartatthesonicpointandintegrateforward,towardtheshock.Eveninthiscase,iter-ationisstillrequiredtondasolutionconsistentwiththeinitialconditionsupstreamofthewave,sincethethermodynamicstateofthesonicpointisnotknownapriori.Forthesolutionofthegoverningordinarydierentialequationsinitializedeigen207,thesolutionforthereactionzonestructureisshowninFig.2.4.Coincidentwiththesonicpoint,thelocalheatreleaserateisseentogotozeroduetoanexactbalancebetweentherateofexothermicheatadditionandendothermicheatremoval.ThisconditionisreferredtoasthegeneralizedChapman Jouguetcondition,atermrstusedbyEyringetal..27].Theconditionofthelocalheatreleaseratebeingzerobehaveslikeaquasi-equilibriumconditionin(2.23),enablingthesolutiontopasssmoothlythroughthesonicpointandproceeddownstreamasasupersonicow(recallthatheatremovalacceleratesasupersonicowawayfromsonic).Thiscaseisshownastheheavy,solidlineinFig.2.4ThesonicpointofthegeneralizedCJconditionisasaddlepoint,soinprincipleitisalsopossibleforthesolutionatthesonicpointtoreturntothesubsonicbranchundertheinuenceofsubsequentendothermicreaction,asshownbythethin,dashedlinesinFig.2.4.Thissolution,however,featuresanonphysicalkinkintheowproperties.Thus,itcouldbesuggestedthatthesolutionthatpassessmoothlyfromthesubsonictothesupersonicbranchisthecorrectone,butthiscannotbeprovenrigorously.Asmentionedpreviously, 44A.Higgins X 0.50.00.51.01.5 singularityCJ EigenvalueCJ Equilibriumsupersonicbranchsubsonicbranch X Distance xMach number M102103104105Distance x102103104105Distance x102103104105Distance x1021031041050.00.51.01.5 singularityCJ EigenvalueCJ Equilibriumsubsonicbranchsupersonicbranch X p/p1102030405060 singularityCJ EigenvalueCJ Equilibriumsupersonicbranchsubsonicbranch X T/T105101520 singularityCJ EigenvalueCJ Equilibriumsubsonicbranchsupersonicbranchq./cpT1sonic pt. in eigenvalue soln.sonic pt. in eigenvalue soln.sonic pt. in eigenvalue soln.sonic pt. in eigenvalue soln. Fig.2.4.ReactionzonestructureofZNDdetonationwithatwo-step,exother-mic/endothermicsystem,showingpressure,temperature,heatreleaserate,andowMachnumberfor RT1=Ea2 =25,=20,2.ThereactionzoneinitializedwithashockbasedontheCJequilibriumsolutionencountersasingular-ityinthenumericalintegration.Theeigenvaluesolutioncanpasssmoothlythroughthesonicpoint,resultinginsupersonicowattheendofthereactionzone(weakdetonation)similarindeterminacyoccursincompressibleisentropicowwhenaninitiallysubsonicowbecomessonicatanareaminimum(i.e.,atathroat).Iftherequirementthattheowpropertiesatthethroatvarysmoothlyisimposed,theowshouldtransitiontoasupersonicsolutionlocallyatthethroat,andfromthere,theowcaneithercontinuesupersonicallyorreturntothesub-sonicbranchviaashockwave,dependingonthedownstreamboundarycon-dition(e.g.,backpressure).Forboththedetonationwithcompetingreactionsandisentropicowwithareachange,theissueofresolvingwhichbranchofthesolutionfollowingthesonicpointisthecorrectsolutionisultimatelydeterminedbyconsideringthedownstreamboundarycondition.Establishinghowtheowexitingthesonic 2SteadyOne-DimensionalDetonations45 CJ EquilibriumQ = 0(inert shock) weakdetonation 00.20.40.60.81 InitialconditionQ = 10(equilibrium)Q = 5(partially reacted)Q = 11.35(partially reacted)Q = 20(exothermic only)v2/v1Generalized CJ(q. = 0)von Neumannstates strong detonation Fig.2.5.Equilibriumandeigenvaluesolutionsforatwo-step,exother-mic/endothermicsystemvisualizedinthe(p,v)plane( RT1=Ea2 =25,=20,surfaceofsuchadetonationmatcheswithadownstreamconditionimposedbyapistonbecomesquiteinvolvedasanumberofpossiblescenariosneedtobeconsidered.ThereaderisreferredtothebookbyFickettandDavis[foracompleteexpositiononthisproblem.FickettandDavisalsoconsiderthecaseoftwoexothermicreactions,whichturnsouttobequalitativelysimilartoasingleexothermicreactionanddoesnotexhibitpathologicalbehavior.Forthemostfrequentlyencounteredcaseofadownstreampistonatrest(correspondingtoadetonationinaclose-endedtube,forexample),theowpassessmoothlytothesupersonicsolutionbeyondthesonicpoint.Inthiscase,theleadingedgeoftherarefactionwavelagsbehindthesonicsurfaceandtheendofthereactionzone,resultinginaregionofuniformsupersonicowbetweentheendofthereactionzoneandtheleadingrarefactionthatwillincreaseinsizeasthedetonationpropagates.ThesescenariosarediscussedfurtherinAppendixTheeigenvaluesolutioncanalsobeinterpretedinthe(p,v)planewiththeuseofpartiallyreactedHugoniots,asrstproposedbyvonNeumann[Fig.2.5,theHugoniotandRayleighlinefortheequilibriumsolutionareshownasdashedlines.TheHugoniotsforthevalueofheatreleaseatanintermediate Formally,aHugoniotisalocusofpossibleequilibriumendstatesforasteadywave,soapartiallyreactedHugoniotisamisnomer. 46A.Higginsvalue(=5)andatthesonicpointoftheeigenvaluesolution(=1135)areplottedasdashed-dottedandsolidlines,respectively.TheRayleighlinefortheeigenvaluesolutionisseentobetangenttothesolidHugoniotcurveatthepointwherethenetrateofheatreleaseiszero(thegeneralizedCJcondition).Inactuality,thereisacontinuousseriesofpartiallyreactedHugoniots,andthecorrectonetouseforthedetonationsolutioncannotbedetermineduntilthekineticrateequationhasbeenintegrated,aswasdoneabove.StartingfromthevonNeumannpoint,asthereactionprogresses,thesolutionproceedsdowntheRayleighlineasindicatedbythedirectionalarrows.Atthesonicpointoftheeigenvaluesolution,thesolutionisindeterminate.Asendothermicreactionsdominateovertheexothermicbeyondthesonicpoint,thesolutionmaycontinuedowntheRayleighline(supersonicbranch),ormayproceedbackuptheRayleighline(subsonicbranch).EitherbranchofthesolutioneventuallyreachestheequilibriumHugoniot.Theupperintersectionpointcanberecognizedasastrongdetonationandthelowerintersectionasaweakdetonation.Asdiscussedabove,theweaksolutionismorelikelytobereal-ized,andthuspathologicaldetonationsareanexampleofaweakdetonationsolution.Ifthereactionzonecalculationisinitializedwiththepost-shockstatecorrespondingtotheCJequilibriumsolution(dashedstraightline),thenasthetangencycondition(sonicow)isencounteredforthersttime,thenetheatreleaserateisstillpositive.Asnetexothermicreactioncontinues,thereisnolongeranintersectionbetweentheRayleighlineandthepartiallyreactedHugoniot,resultinginthesingularityencounteredinFig.2.4.Thus,itisnotpossibletoconstructatrajectoryofpartiallyreactedstatestoreachtheCJequilibriumsolution.DetonationsforwhichtheequilibriumCJdet-onationsolutionmaynotbethecorrectsolution(orpermissiblesolution)duetocompetingeectsinthereactionzonemayoccurinsystemswithrealchemistryaswell(Sect.2.52.4DetonationswithSourceTermsInordertodiscusslimitstodetonationpropagation,lossesmustbeintroducedintothegoverningconservationequations.InasystemwithoutlossesandgovernedbyanArrhenius-typereactionrate,detonationpropagationisalwayspossibleduetothefollowingmechanism.AnArrhenius-governedsystemwillinevitablyreacttoequilibrium,andthetemperatureincreasefromevenaweakshockwavewillacceleratethereaction,resultinginawaveofexothermicenergyreleasetravelingwiththeshocksomedistancebehindit.Inthecaseofaveryslowreaction,thisfrontofexothermicitymaybespatiallyseparatedfromtheshockbyvastdistances,butintheabsenceoflossessuchasheattransferorfriction,theenergyreleasedwilleventuallyfeedintosupportingtheshock,ultimatelyresultinginadetonation.(RecallthataCJdetonationistheminimumvelocityallowedforasteady,compressivecombustionwave; 2SteadyOne-DimensionalDetonations47lowervelocitycombustionwavesarenotpermittedbytheconservationlaws.)ThisconceptissometimesreferredtointheRussiandetonationliteratureasKharitonsprinciple,namelythatanymediacapableofexothermicreactioniscapableofsupportingdetonationwavepropagationintheabsenceoflossesosses72].Thus,anydiscussionofthelimitstodetonationpropagationmustincludetheeectsoflosses.Thesteady,one-dimensionalmass,momentum,andenergyequationsincludingfrictionandheattransfersourcetermsinthewave-xedreferenceframeare)=0(2.26)(2.27) (2.28)whereisasourcetermofmomentumandisasourcetermofenergy.Thevelocityisthevelocityofthewallinthewave-xedframe,whichisequalinmagnitudetothevelocityofthewaveinthelaboratory-xedframe,.Aswrittenhere,andarethevolumetricsourceterms,withunitsof[Nm]and[Wm],respectively.Amasssourcetermcouldalsobeincludedtoaccountfor,forexample,masslossintoaporouswall;however,thiseectisusuallytreatedbyintroducingareadivergenceintothegoverningequations,asdiscussedinSect.2.6.Thesemomentumandenergysourceswillberelatedtowallfrictionandheattransfercoecientsbelow.Notetheappearanceofthefrictiontermintheenergyequation,representingtheworkdonebyfriction.ThesignicanceofthistermwillbeelaborateduponinSect.2.4.2below.FollowingthedevelopmentofSect.2.2,adierentialequationfortheowvelocityinthereactionzonecanbefound dx=q cpT+q cpT+f(u1(1)u) c2 (2.29)Notethatif=0and=0,(2.29)revertsbackto(2.16).Heattransfertothewallisaheatloss(0),soinspecting(2.29)revealsthattheeectofheatlossissimilartothatofendothermicreactionsstudiedintheprevioussection.HeatlosseswillresultinthedetonationpropagatingatspeedslessthantheidealCJdetonationvelocity(i.e.,adetonationwithoutlosses),anddeterminingthesolutionwillnecessitateiteratingonthepropagationvelocityuntilaregularsolutionofthereactionzonestructurecanbefound.Theeectoffrictionisnotasintuitive,duetothetermsofmixedsigninvolving2.29);however,itwillbeshownthatfrictionalsoresultsinavelocitydecitincomparisontotheidealCJvelocity. 2SteadyOne-DimensionalDetonations57verylarge(i.e.,beyondvaluesthatcorrespondtorealreactivesystems)inordertoseethisconvergence.InSect.2.6,thesamerelationrelatingvelocitydecittoactivationenergywillbefoundtoapplytodetonationswithfrontcurvatureduetolateralowdivergencefromyieldingconnement.Detonationswithlargefrictionalandheattransferlosses,aswouldbeencounteredinporousmediaforexample,havebeenextensivelystudiedthe-oreticallybySivashinskyandcolleaguesinrecentyears[].Theirworkhasfurtherelucidatedthestructureofthereactionfrontandclassi-edthepossiblemodesofpropagation,particularlylowvelocity(includingsubsonic)regimes.Theirmodeling,similartothatpresentedhere,usedasingle-stepArrheniuskineticsreactionmechanism.Asdiscussedinthenextsubsection,thisreactionmodelislikelynotrelevanttotheactualmechanismofburninginreactivewaveswithlargelosses.Modelsthatattempttoincor-poratethecontributionofturbulentcombustiontothereactionmechanismbyusinggreatlyexaggeratedvaluesoftransportproperties(e.g.,eectivetur-bulentdiusivity,etc.)mayprovideafuturedirectiontolinkthesemodelswithexperimentalresults[2.4.5ExperimentswithLossesGaseousdetonationsinchannelsthatexhibitlargevelocitydecitsduetomomentumandheattransferlossestowallroughnessorobstacleshavebeenextensivelystudiedandarereferredtoasquasi-detonations.Quasi-steadypropagationatvelocitiesaslowas50%oftheidealCJvelocityhasbeenobserved.Reviewsofresultsofthesestudiescanbefoundin[]andChap.of[].Itisunlikelythatplanarshock-initiatedhomogeneousreactionscon-tributesignicantlytotheenergyreleaseinsuchdetonations.Calculationsperformedwithdetailedchemistryshowthatthereactionratesforthelowshockvelocitiesinvolvedaremuchtooslowtoresultinexothermicreactionsonthetimescalesoftheobservedquasi-detonations.AseminalstudybyShchelkinhelkin78]suggestedthatshockreectionoobstaclesinthetubemaygeneratelocalhotspotsthatinitiatereactionandthusenablethedetonationtocontinuepropagatingatspeedsforwhichaplanarshockwouldnotbeofsucientstrengthtosustainpropagation.Muchoftheframeworkforexplainingdeto-nationphenomenaingaseousandcondensedphaseexplosiveshassincebeenbuiltaroundthishotspotidea.Inaddition,itislikelythatinteractionsofthepost-shockowwiththeobstacles,theboundarylayerthatformsonthetubewall,andtheturbulentnatureofthequasi-detonationfrontitselfallcontributetoburningthemixtureandsustainingthefront.Themechanismofpropagationofveryhighspeed(300ms)turbulentameshasnotbeenconvincinglyelucidatedandcurrentlycomprisesanomanslandbetweenpremixedturbulentcombustionanddetonation,whichincludesthetransitionbetweenthetwo(deagrationtodetonationtransition)[].Assuch,mod-elstoaddressthereactionmechanismareadhocandsemi-empiricalinnature 2SteadyOne-DimensionalDetonations59aregeometrydependent,asseenintheresultswiththesquaretubewithstaggeredpillars,whichwhileexhibitingacriticalvelocitydidnotexhibitatransitiontothelowvelocitychokingregime.SimilarstudiesofdetonationsingaseousmixturesllingtheinterstitialspacesinpackedbedsofinertsphericalbeadsbyMakrisetal.[]andPinaevandLyamin[]failedtoidentifyacriticalvelocityforalargenumberofdierentexplosivemixtures,withacontinuousspectrumofpropagationvelocityfromtheidealCJvelocitydownto30%oftheCJvelocity.Itislikelythattheroleofturbulentmixing-drivencombustionwavesaccountsforthegeometry-dependingvelocitydecitandcriticalbehaviorthatcannotbepredictedbythesimplehomogeneousreactionmechanismswithexponentialtemperaturedependenceusedinthischapter.2.5SystemswithRealChemistryInordertohaveamoreaccuratemodelforrealsystems,itisnecessarytotakeintoaccountthedetailsofthechemicalreactions,ratherthansimplytreatingtheenergyreleaseofreactionasexternalheatadditionaswasdoneinpriorsections.Inthissection,amodelofasteady,one-dimensionaldetonationinareactingsystemofidealgaseswillbedeveloped,followingthedevelopmentsfoundin[].Thisanalysisbeginswiththesamedierentialformoftheconservationequations(2.1) (2.3)andadditionalconservationequationsforeachindividualchemicalspecies(2.40)sincespecieswillbeproducedandconsumedwhilechemicalreactionsproceed.subscriptin(2.40)denotesaparticularchemicalelementorcompound.Thetermistherateofspeciesproductionviachemicalreaction(units:kmol/m-s),andisthemolecularweightofspecies.Itisconvenienttointroducethemassfractionofaspecies ,whereisthedensityofthemixture.UndertheassumptionoftheDaltonmodelofpartialpressure,theidealgaslawappliestoeachindividualspecies .Theaveragemolecularweightofthemixture(whichwill,ingeneral,notremainconstantasthemixturereacts)isgivenby W\biYi (2.41)Theenthalpytermcontainsboththesensibleenthalpyandthelatententhalpyofformation.Thus,itisnotnecessarytointroduceaheatreleasetermintotheenergyequationtoaccountforexothermicchemicalreaction.Specically,isgivenby(2.42) 64A.Higginswhererefisthereferencepressureusedindeningtheequilibriumconstantbasedonpartialpressures.Equilibriumconstantsarederivedfromthermodynamicdataasfollows:=exp (2.67)where¯istheGibbsfunctiononapermolebasisofspeciesevaluatedatthetemperatureandatthereferencepressureref=1atm.Thus,theequi-libriumconstants,inbeingderivedfromfundamentalthermodynamicdata,areknownwithmuchgreatercondencethankineticrateconstants.Thisapproachthenensuresthattheoverallkineticmechanismisconsistentwiththehigher-condenceequilibriumconstants.Aconsequenceofthisassumptionisthatitispossibletostartwithacompletelyarbitraryorincorrectreactionmechanismandstillreachthecorrectequilibriumcompositionofareactinggasmixture.Thus,correctlyreproducingtheCJdetonationvelocityviaaZNDcalculationwithdetailedchemistryshouldnotbetakenasvalidationofthekineticmechanism.Theoverallconversionoffuelandoxidizerintoproductsisdescribedbyakineticmechanism,consistingofelementaryreactions.Formostcombustiblemixtures,itisnecessarytoconsidernumerouspossiblereactions.Evenasim-plesystemlikehydrogen/oxygenistypicallymodeledwith20orsoelemen-taryreactions,whilemechanismsforhydrocarbonfuels(e.g.,methane)canconsiderreactionsnumberinginthehundredsorthousands.Foramechanismconsistingof,...,Melementaryreactionsthatdescribesthereactionof,...,Nspecies,theoverallproductionrateofspeciesisgivenby(2.68)(2.69)whereisthestoichiometriccoecientofspeciesintheforwardreactionandisthecorrespondingstoichiometriccoecientforthebackwardreac-tion.Ifaspeciesisabsentfromareaction,itsstoichiometriccoecientisThetimerateofchangeofconcentrationisoftenexpressedinthecom-bustionliteratureas (2.70)Thisexpressionisstrictlyonlyvalidforaconstantvolume(density)reac-tion.Ingeneral,reactingowsarevariabledensity,sospeciesconcentrationscanchangeduetochangesindensityaswellasreaction,andthus(2.70)is 66A.HigginsTable2.1.Carbonmonoxide/oxygenreactionmechanism ReactionAnE(kJ/kmol) CO+O+M+M1.80.009,970CO+O+O2.50.00200,000O+O+M+M1.21.000 kmolkmolroleofhydrogeninconvertingtheCOintoCO.Thus,inanyrealsystemwitheventracecontaminationofhydrogen,water,orhydrocarbons,themechanism2.72) (2.74)isnotthedominantreactionpath.Forthepurposesofamodelsystemtoexplorenumerically,however,thedryoxidationofcarbonmonoxideisconvenienttouse.InordertoinitializethecalculationofthereactionzonestructureatthevonNeumannpoint,itisnecessarytospecifythepropagationvelocityofthedetonationwave.Thiswasdoneintwodierentways:anequilibriumsolu-tionbasedonacontrolvolumeenclosingthewaveandaZNDsolutionwhichthestructureofthereactionzoneissolved.Theequilibriumsolutionbasedonacontrolvolumewasdeterminedthroughiterationupontheinte-gralconservationlaws(2.1) (2.3)assumingchemicalequilibriumattheexitplaneuntiltheminimumwavevelocitysolutionwasfound.Thereactionzonestructurewasnotconsideredinthiscase.Thespeedofsoundwasnotexplic-itlyintroducedinthesecalculations,butthesolutionfoundcorrespondstosonicoutow(i.e.,owvelocityequalstheequilibriumspeedofsound).Thissolutionmethodologycanbeshowntoagreewiththatusedinwell-knownequilibriumprogramssuchastheNASACEAprogram[],andgeneratesthesameresultswithinnumericalprecision.TheZND-basedsolutionwasfoundbynumericallyintegratingthereactionzonestructureusingthe(2.58) (2.71).Theinitialvelocityofthewavewasiter-ateduponuntilasolutionthathadsonicoutowandthatdidnotencounterasingularitywasfound.Notethatthesonicoutowconditionfoundisthatdenedbyusingtheequilibriumspeedofsound.Theoutowwithrespecttothefrozenspeedofsoundwasstillsubsonic(Mach0.963).Therefore,thissolutiondoesnotsatisfythegeneralizedCJcondition(2.59TheresultsofthetwosolutionmethodologiesarecomparedinTable2.2Thepropagationvelocityofthedetonationwavefoundbythesetwomethodsagreestosixsignicantdigits,andtheowpropertiesattheexitstateagreetowithinveorsixsignicantdigits.Thus,itcanbeconcludedthatthesetwomethodsndthesamesolutionforthedetonationwave.ThestructureofthewaveisshowninFig.2.10.Thereactionzonelength,asdenedbyidentifyingthelocationofmaximumthermicityortheinectionpointintemperature,isontheorderof10 15cm.However,thesoniccondition(usingtheequilibriumsoundspeed)isonlyapproachedasymptotically.Thus, 2SteadyOne-DimensionalDetonations69existsinthiscasethatpermitsthesolutiontosatisfythegeneralizedCJcriterion.Thisresultisduetothefactthatthethermicityparameterisalwayspositiveandonlyapproacheszeroasymptotically.Inorderforthesolutiontopassthroughsonicviaasaddlepoint,thethermicitymustpassthroughzero.Thus,forthecarbonmonoxide/oxygensystemdiscussedhere,thereisnoambiguitysincetheequilibriumandtheZND-basedmethodsgeneratethesameuniquesolution.2.5.3Hydrogen/ChlorineSystemIdenticationofarealcombustiblemixturethatexhibitsthetypeofpatho-logicalbehaviordiscussedinSect.2.3isaninterestingproblemthathasbeenthesubjectofperiodicinvestigationsincetheintroductionoftheZNDmodelinthe1940s.ZeldovichandRatner[]pointedoutthatthereactionofHandCltoformHClcanoccurviatheNernstchainreactionmuchmoreread-ilythanthedissociationofCl,whichhasarelativelyhighactivationenergy.Thus,thehighlyexothermicreactionformingHClmaybefollowedbyanendothermicdissociationreactioninCl,resultinginthetypeofexother-mic/endothermicreactionnecessaryforpathologicalbehavior.Subsequentstudiesofexperimentalsystemsexhibitingpathologicalbehaviorhavetendedtofocusonthissystem.TherstdetailedchemicalkineticcalculationsofaZNDdetonationin/ClwereperformedbyGu´enocheetal.[]usingthemechanismgiveninTable2.3.Thesecalculationsarereproducedhere.Afuel-lean(chlorine-rich)mixturewithfuelequivalenceratio66atrelativelylowpres-sure(33kPa)wasselectedhereforasamplecalculationinordertoaccentuatethedierencebetweentherapid,exothermicformationofHClandtheslowerdissociationoftheexcessCl.Thegoverningdierentialequa-tions(2.58) (2.71)wereintegratedcoupledwiththekineticmechanisminTable2.3.TheinitialshockvelocitywasiterateduponuntilasolutionthatTable2.3.Hydrogen/chlorinereactionmechanism ReactionAnEkmol)(kJ/kmol) H+H+M+M1.01.000HCl,Cl,Cl1.000H0.600H2Cl+M62.07238815H,Cl,HCl,H2.07238857ClHCl+MH+Cl+M62.00427765H,Cl,HCl,H,ClCl+HHCl+H40.0022H+ClHCl+Cl60.684 kmol 70A.HigginsTable2.4.Hydrogen/chlorinedetonation Initialcomposition(Moles)H Initialstate(kPa)3(K)300(ms)278 DetonationsolutionEquilibriumEigenvalue(ZND) (ms)1,320.71,527.34.7355.476vonNeumannstate(kPa)86.469116.0618.06634.852(K)1,374.11,724.4(ms)232.96251.88(ms)586.81655.230.39700.3844Chapman Jouguetstate(kPa)47.07360.30014.13618.108(K)2,075.942,989.09(ms)748.4883.3(ms)789.0883.3(ms)748.4N/A0.94851.00001.0000N/A passesthroughthefrozensonicpointwasidentied.ThissolutionispresentedinTable2.4andFig.2.12,showingthethermodynamicproperties,speciesconcentrations,thermicityparameter,andtheowMachnumber(usingthefrozenspeedofsound).AshypothesizedbyZeldovichandRatner,theH/Clsystemdoesexhibitanovershootintheheatreleasefollowedbyanendother-micphase.Thisismostclearlyseenbyexaminingthetemperatureandthethermicityparameter,whichpassesthroughzeroandbecomesnegativeatthesamepointwheretheowbecomesfrozensonic,asrequiredbythegeneralizedCJcondition.(Notethefactthatthethermicitybecomesnegativepreventstheuseofalog-scaleonthe-axis,incomparisontoFig.2.10.)Thehistoryofspeciesconcentrationsthroughthereactionzoneveriesthattherapidforma-tionofHClfollowedbyaslowerdissociationofClintoClisthesourceoftheexothermic/endothermicnatureofthereaction.Thissolution,resultingfromiterationuponthereactionzonestructureuntilatrajectorythatsatisesthegeneralizedCJconditionwasfound,istheeigenvaluesolution.Theeigenvaluesolutionfoundaboveiscomparedtotheequilibriumsolu-tion,suchaswouldbefoundviatheNASACEA[]orotherchemicalequilibriumsoftware,inTable2.4.Asignicantdierencebetweenthetwosolutionsisfound,witha15%discrepancyinthedetonationpropagationvelocitieswiththeequilibriumvelocitybeinglower.Thisresultisunlikethat 2SteadyOne-DimensionalDetonations71 Mole Fraction10-310-210-1100Cl2H2ClH X 100HClsonic surface Flow Mach Number (frozen sound speed)0.20.40.60.81.01.21.41.61.8sonic (frozen) Thermicity (1/s) Distance (m)Pressure (atm)Temperature (K)10-410-310-210-1100Distance (m)10-410-310-210-1100Distance (m)10-410-310-210-110000.511.521600180020002200240026002800300032003400PressureTemperature Fig.2.12.StructureofHdetonation,showingpressure,temperature,molefractions,thermicity,andowMachnumber.ThelocationofthesonicpointisdenotedasaverticaldashedlineobtainedwithCO/Odetonationsconsideredinthepriorsection,forwhichtheequilibriumandZNDapproacheswereseentogeneratethesamesolution(withinnumericalprecision).IfaZNDcalculationoftheH/Clreactionzoneisinitializedwiththepost-shockvonNeumannconditionsfortheCJequilib-riumsolution,asisdoneinFig.2.13,thecalculationencountersasingularity.Thereactionzoneisnowlongerduetothelowerpost-shocktemperature,butwhentheexothermicreactionbeginstoreleasesignicantheatintotheow,itresultsinsonicowbeingencounteredbeforethethermicitygoingtozero,hencecausingthesingularity.Qualitatively,thisisidenticaltothebehaviorseeninSect.2.3withanarticiallyconstructedtwo-stependother-mic/exothermicsystem.Indeed,anyattempttoinitializeasolutionwithashockvelocityevenincrementallybelowtheeigenvaluesolutionfortheH/Clsystemresultsinasingularity.Solutionsinitializedwithafastershockremainsubsonicwithrespecttothefrozenspeedofsound(i.e.,thestrongdetonationsolution).Finally,notethatitisnotpossibletodeneanequilibriumsoundspeedforthe(nonequilibrium)sonicpointoftheeigenvaluesolution. 76A.Higginswavefrombehindanddisruptingthereactionzone.However,asadetona-tionpropagates,thegradientofexpansionbehindthewavebecomesmoregradual,andthusthefrequencyofrarefactionwavesmightbeexpectedtoapproachthelow(equilibrium)limit.Further,whiletheinitialleadingedgeofacenteredrarefactionwouldpropagateatthefrozenspeedofsound,thisacousticwaveisquicklyattenuated(decaysexponentially)andthemajorityoftherarefactionisgovernedbytheequilibriumspeedofsound.ThisaspectofrarefactionspropagatinginreactiveowwasexploredindetailbyWoodandParker[].Ifthisisthecase,thentheequilibriumsolutionwouldagreewiththeconceptualpictureoftheCJdetonationbeingisolatedfromdownstreamdisturbancesbyasonicplane.Forasystemwithpathologicalheatrelease,suchasthehydrogen/chlorinesystemconsideredinSect.2.5.3,itisnotpossibletoobtainasolutionforthereactionzonestructurethatisinitializedwiththeCJequilibriumvalueofdet-onationspeed(seeFig.2.13).Thiscasecanbevisualizedonthe(p,v)planebytheinabilityofasequenceofintermediateHugoniotstoprovideapathalongtheRayleighlinetoastateoftangencytotheequilibriumHugoniot(seeFig.2.5).Theonlypermittedsteadysolutionwithasonicpointistheeigenvaluesolutionwithafrozensonicpointembeddedinthesolutionandanexitowthat,withrespecttotheequilibriumHugoniot,isaweakdeto-nation.Similarly,inanysystemwithlossessuchasheattransferorfriction,asdiscussedinSect.2.4orwithlaterallydivergentow,aswillbediscussedinSect.2.6,itisthefrozensoundspeedthatdenesthesaddlepointoftheeigenvaluesolution.Thissituationgivesrisetoanapparentparadox,whereinthelimitingsolu-tionasthelossmechanismdecreasestozeromaynotconvergetotheideal,planarsolution,sincetheformerisdenedbythefrozenspeedofsoundandthelatterusestheequilibriumspeedofsound.Forexample,forthecaseofadetonationinatubewithlossesatthewalls,astheradiusofthetubeincreasestoinnity,thesolutionforthedetonationvelocitywillnotagreewiththeplanarsolution(i.e.,lim).Inordertoresolvethisapparentinconsistency,apossiblestrategywouldbetosolvethefull,unsteadyEulerequationswithoutimposingaparticularcriterion,andseewhichsolu-tionevolves(thisapproachwasdonebySharpeandFalle[]forpatho-logicaldetonationsandbyDionneetal.[]fordetonationswithfrictionandheattransfer,asdiscussedinSect.2.4.3).SuchacalculationwasperformedbySharpe[]foramodelsystemwithasingle-stepreversiblechemistryoriginallyproposedbyFickettandDavis[](FickettandDavisconsideredasystemwithzeroactivationenergy,whileSharpeconsideredasystemwithlowactivationenergythatgaveastableZNDsolution).Sharpe[]showedthat,foraplanardetonationinitiatedbyanoverdrivenblastwaveintheabovesystem,afteralongpropagationtime,thewavevelocityandreactionzonestructureapproachedthatofanequilibriumsonicCJdetonation.However,ifevenaninnitesimaldegreeoflosswasintroduced(curvature,inthecaseofSharpescalculations),thelong-termevolutionofthesolutionconverged 78A.Higginswhichthecriticaldimensionisrstencountered.Ingaseousexplosivescon-tainedinrigidtubes,near-limitbehaviorismorecomplex,sincethewavecaninteractwiththetubewallinordertosustainpropagationintransientmodesknownasspinningandgallopingdetonations(seediscussioninChap.of[Thevelocitydecitinnite-sizedchargesandtheexistenceofacriti-caldimension(usually,thediameterofacylindricalcharge)areheavilyuti-lizedinresearchondetonationwavesincondensed-phaseexplosivesasameanstoprobethereactionzonestructureandthermodynamicpropertiesofthedetonationproducts.Duetotheextremelyshortreactiontimescalesincondensed-phasedetonations(typically,sub-microsecondtonanosecond),theopaquenatureofdetonatingmedia,andtheextremepressuresgenerated,insitumeasurementsofanydetonationpropertiesareextraordinarilydicult.Asaresult,almostallmodelsforcondensed-phaseddetonationsutilizedataderivedfromthevelocitydecitand/orthecurvatureoftheshockfrontasthechargediameterisdecreased,ormeasurementofthecriticaldiameteratwhichdetonationfailureoccurs.Theradialexpansionofdetonationproductsinacylindricalchargeconnedwithaductilematerial(e.g.,copper)isalsothebasisofmostsemi-empiricalmodelsfortheequationofstateofthedetonationproducts.Fordetonationsingas-phasemediaontheorderofatmosphericpressure,perfectlyrigidconnementispossible,forexample,usingasteel-walledtube.However,theperipheryofthegaseouschargestillinuencesthedetonationwaveviafrictionandheattransfertothewall.InSect.2.4,theseeectsweretreatedasvolumetriclossesthatwerespreaduniformlyacrossthecrosssectionofthetube.Inreality,theinuenceofthewallisconveyedtothedetonationowviaaboundarylayerregionnearthewall.Thegrowthoftheboundarylayerresultsinadivergingowinthereactionzone,qualitativelysimilartothedivergingowthatoccursinacondensed-phasedetonationduetoyieldingconnement.Itmayappearcounterintuitivethatgrowthofaboundarylayeralongthewallresultsinadivergingowinthedetonationreactionzone;notethatinthewave-xedreferenceframe,thewallshavetheeectofacceleratingtheowwhilealsocoolingandincreasingthedensityofgasintheboundarylayer.Bycontinuity,thiseectrequiresthatthecoreoftheowdivergesoutwardtoaccountforthemasseectivelyremovedbytheboundarylayer.BoundarylayersofthistypearesometimescallednegativeboundarylayersWithinthecontextofaquasi-one-dimensionalapproximation,detonationswithdivergentowcanbetreatedwiththereactionzoneequationsderivedpreviouslyinSect.2.2.Inparticular,(2.10),reproducedhereslightlymodied dx=q cpT\nu1 AdA dx (2.75)modelstheeectofdivergingowviathe AdA term.Inthissection,thesteadyreactionzonestructureofdetonationwaveswithdivergingowisfurther 80A.Higgins(0)Ld))whereisthelengthofthereactionzone,thentheareadivergencetermsdierbyanumericalfactoroftwoforthetwogeometries2-DSlab: AdA dxt(x) (0)(2.80)AxisymmetricTube: AdA dx2d(x) (0)(2.81)Thismeansthatthesolutionforthereactionzonestructureinthetwogeome-triesshouldbethesame,providedthediameteroftheaxisymmetriccylinderisscaledbytwicethethicknessofthe2Dslab.Earlymodelsfordetonationinnite-diameterchargesbyJones[]andEyringetal.[]usedphenomenologicaldescriptionsforthestreamtubeareadivergence(i.e.,nozzleowmodels).Whilenotrigorous,thesemodelsareofinterestintheirprovidingaphysicalpictureoftheoweldsthatresultfromtheboundaryofthechargeexpandingoutwardastheexplosivereacts.ThemodelsdevelopedbyJonesandelaborateduponbyEryingetal.assumedaPrandtl Meyer(P M)expansionfanoriginatingwhereanormaldetonationencounteredtheedgeofthecharge.TheinitialstatewastakenastheCJstatefortheideal,constantareadetonation(notethatusingthesubsonicvonNeumannstateisnotanoptionsincetheP Mfunctionisonlydenedforsupersonicow).Foranunconnedcharge,theP Mfanattheedgewasmatchedtoastreamtubecontainingthecoreofthedetonationow.Foraheavilyconnedcharge,theP Mfanwasmatchedtoanobliqueshocktransmittedintotheconningmaterialtodeterminethedivergenceangle,whichwastakenasconstant.Eyringetal.wentontodevelopheuristicmodelsincorporatingthefactthat,iftheowattheboundaryofthechargeisdivergingoutwardfollowingtheleadingshock,theshockfrontitselfcannotbeatandmustbeobliqueattheboundary.Inotherwords,theleadingshockfrontiscurved(normalonthecentralaxisofthechargeandincreasinglyobliquetowardtheedges),similartothemeniscusofaliquidsurfaceinacapillarytube.Eyringetal.werecarefultopointoutthatfrontcurvatureisanecessaryconsequenceofdivergingow;curvatureandowdivergencearedierentmanifestationsofthesamephenomenon,notseparateeectsthatshouldbesuperimposedinmodels.Theoreticalinvestigationsintothe1960scontinuedtopresupposefunctionalformsforthestreamtubeareaprole,oftenoutofanalyticconvenienceratherthanfromphysicalconsiderationss26,100].2.6.2RadialFlowDerivativeBeginningwiththeworkofWoodandKirkwood[],amorerigorousapproachtosolveforthereactionzoneofadetonationwavewithdivergentowwasdevelopedthatexaminedthetwo-dimensionalow(eitherrectangu-laroraxisymmetric)alongthecentralaxialstreamlineofthereactionzone. 2SteadyOne-DimensionalDetonations81Utilizingthefactthattheowissymmetricaboutthisline,thecontinuityequationfortwo-dimensional,steadycompressibleow=0(2.82)canbesimpliedforrectangularcoordinates x+(v) =0(2.83)sincethetransverseowvelocityiszeroalongthisstreamline,asfollows: x+v (2.84)Notethat,whilethetransversevelocityiszeroalongthecentralstreamline=0),thederivativeofthevelocityintheradialdirectionhasanonzerovalue .Likewisethecontinuityequationforaxisymmetricowincylindricalcoordinates x+1 rv =0(2.85)specializedtothecentralstreamlinevialHopitalsruleyields x+2v (2.86)-momentumequationinrectangular uv y=p (2.87)andcylindricalcoordinatesru ruv r=rp (2.88)bothrevert(viasymmetry)tothefamiliarformofthemomentumequationwhenappliedalongtheaxialstreamline x+uu (2.89)Returningtocontinuity,(2.84)and(2.86)canbewrittenas x+v (2.90)wheredenotesthetransverse-directionintherectangulargeometryandradial-directioninthecylindricalgeometry,andhasthevalueof1and 82A.Higgins2fortherectangularandcylindricalgeometries,respectively.Bycomparing2.90)with(2.4),thederivativeofthetransverse/radialvelocityterm( canberelatedtotheareadivergenceofastreamtube AdA dx= uv (2.91)Thisequivalencecanalsobedemonstratedbyconsideringanarbitrarilysmallstreamtubethatenclosestheowalongthechargeaxis,andusingthederiva-tiveoftheradialowvelocitytoapproximatethedivergenceofthestreamtubeboundary.Asthestreamtubeshrinkstotheaxis,thecorrespondence2.91)becomesexact.2.6.3ShockFrontCurvatureThederivativeoftheradialowvelocitycanalsoberelatedtotheradiusofcurvatureoftheleadingshockfrontbyusingthegeometricconstructionintheshock-attachedreferenceframeshowninFig.2.16.Theowvelocityapproachingtheshockisthedetonationpropagationvelocity().Notethatthisconstructionappliestothe2Dslabandaxisymmetricgeometriesequally.Usingthefactthatthecomponentofowvelocityparalleltoashockfrontdoesnotchangeastheowcrossestheshock,asrequiredbyconservationofmomentum,itispossibletoexpresstheradialcomponentofvelocityas(2.92) DDu\\ =D sin\bu\t = D cos\bu\tv\b u\\centerlineRshock frontvon Neumann point x y, r two-dimensional slabaxisymmetric cylinder Fig.2.16.Geometricconstructionrelatingshockfrontradiusofcurvaturetothederivativeoftheradialowvelocity rorv atthecenterlineimmediatelybehindtheshock 2SteadyOne-DimensionalDetonations83Performingapartialdierentiationofthevelocitywithrespecttotheangle shock(cos2 shock(2.93)wheretheshocksubscriptdenotesthatthedierentiationwasperformedalongtheshockfront.Thedierentiationcanbeconvertedtoadierentialwithrespectto(denotedas)asfollows: shock shock shock shock (2.94)Takingthelimitapproachingthecentralaxis (0) (2.95)where(0)istheaxialvelocityatthevonNeumannpointalongthecentralaxis.Thus,theradiusofthecurvatureoftheshockfrontisdirectlyrelatedtothederivativeoftheradialowimmediatelybehindtheshockfront.ThisrelationappliesstrictlyonlyatthevonNeumannpoint(i.e.,immediatelyaftertheleadingshock);however,lackingfurtherinformation,thisderivativeisoftentakenasconstantthroughthereactionzone.Theshockradiuscanberelatedtothecurvatureoftheshockfrontasfollows: (2.96)whereagainis1forthetwo-dimensionalslabgeometry(cylindricalcurvatureoftheshockfront)and2fortheaxisymmetriccylindergeome-try(sphericalcurvatureoftheshockfront).Thefactthat,foralocallysteadydetonationfront,theshockcurvatureuniquelydeterminestheeigenvaluevelocityofpropagationprovidesthemeanstoconstructthedetonationfrontshapeandtrajectoryasthedetonationpropagates,forexample,throughacomplexchargegeometry.Thistechnique,calledDetonationShockDynamicsisthesubjectofChap.ofthisvolume.2.6.4ConnementInteractionviaNewtonianTheoryInordertoassociatethesedivergentowmodelswithexperimentalresultsormakequantitativepredictionsofvelocitydecitsorcriticaldiameter,itisnecessarytolinktheowdivergencetotheoveralldimension(diameterorthickness)ofthechargeandthepropertiesoftheconnement.Forcondensed-phasedetonations,solvingforthisinteractioncanbechallenging;thistopiciselaborateduponinChap.ofthepresentvolume.Asanillustrativenumericalexamplerelevanttogaseousdetonations,asimpleNewtonianmodelfortheinteractionofthedivergingowinthereactionzonewiththeconnementwillbedevelopedfurtherinthissection.Beinganozzleow-typemodel,itdoesnotexplicitlyincludethecurvatureoftheshockfront.However,this 84A.Higginsmodel(originallyproposedbyTsugeetal.[])isinstructiveinthatittreatstheevolvinginteractionofthereactingowwiththeconnementviaananalyticallytractablemethodwithoutresortingtoempiricalinputoranassumedformulafortheareadivergence.TheNewtonianmodelforhypersonicowassumesthataowencounteringaninclinedsurfacelosesthecomponentofvelocitynormaltothesurfacebutretainsthetangentialvelocity.Inotherwords,aowencounteringaninclinedsurfaceslidesalongthesurface,andthechangeinmomentumuxoftheowdeterminesthatthepressureonthesurfacemustvaryas(2.97)whereisthesurfaceinclinationangletotheowwithfreestreamdensity,andvelocity.OriginallyproposedbyNewton,thisowmodelhasbeenshowntoberemarkablyaccurateinpredictingsurfacepressuresforslenderbodiesinhypersonicow[].Themodelisinvokedheretotreattheowoftheconnementmaterialasitencounterstheexpandingowofreactinggas,therebylinkingthepressureofthereactingowtothedivergenceangleofthestreamtubeenclosingthatow.Sincethestreamtubecannotsupportapressuredierence,thereactingowmustlocallymatchthepressureoftheconnementandtherebytheslopeofthestreamtubeboundary.Using2.97)fortheowofconnementmaterial dx2 1+\ndz (2.98)wheredenotesthepropertiesoftheconnementbeforeinteractionwiththedetonationwaveandiseithertheradiusorthehalf-thicknessthestreamtube.Solvingfortheslopeofthestreamtube dx=\f\r\r p(x)pc cu2c 1p(x) (2.99)Thisexpressionisusedtondtheareadivergencetermasafunctionofthelocalpressureinthestreamtube2-DSlab: AdA dx=t t=y y=1 y\f\r\r p(x)pc cu2c 1p(x)pc (2.100)AxisymmetricTube: AdA dx=2d d=2r r=2 r\f\r\r p(x)pc cu2c 1p(x)pc (2.101)Theseexpressionsfor AdA canbeuseddirectlyintheODEgoverningthereactionzonestructure(2.75).Sincepressurenowappearsexplicitly,thisODEmustbeintegratedcoupledtothemomentumequation(2.5)reproducedhere 2SteadyOne-DimensionalDetonations85 dx=udu dx=m Adu (2.102)whichcanberelatedtothelocalstreamtubedimensionasfollows:2-DSlab: dx=1u1y1 ydu (2.103)AxisymmetricTube: dx=1u1\br1 r\t2du (2.104)whereandarethedensityandvelocityupstreamofthedetonation)andandaretheinitialhalf-thicknessandradiusoftheexplo-sive,respectively.ThissetofODEswasintegratedtoobtainthestructureofadetonationwithyieldingconnement.Thepropertiesoftheexplosivewerethesamethathavebeenusedpreviouslyinthischapter(=10,andasingle-stepArrheniusreactionwith =25).Theinertconnementwasassumedtobeatthesameinitialpressureastheexplosive,butwithadensity2.5timesgreaterthantheexplosive().Thisdensityratioapproximatelycor-respondstothedensityratioofairtostoichiometrichydrogen/oxygen,whichwillbeusedasanillustrativeexperimentlaterinthissection.AsexpectedfromtheformofthegoverningODE(2.75),wheretheeectofareadivergencefromtheyieldingconnementisseentocompetewithexothermicheatrelease,itisnecessarytoiterateuponthedetonationvelocitytondaneigenvaluesolutionthatcanpasssmoothlythroughthesonicpointwithoutencounter-ingasingularity.Aswasseenpreviouslywiththeeectofheattransferandfriction,thereisacriticalamountoflossthatthedetonationcansustain,inthiscase,resultingfromtheexplosivechargebeingtoothinandlosingtoomuchmomentumtothedivergenceoftheow.Forchargesthinnerthanthiscriticalthickness,nosteadysolutionwithasonicpointcanbefound.Thestructureofthereactionzoneforthecriticalslabthicknessatwhichfailureoccurs(i.e.,atthecriticalturningpoint)isshowninFig.2.17asthicklinesincomparisontotheidealCJsolutionforaninnitethicknesscharge(thinlines).Asmallschematicdonetoscaleisincludedtoshowtheactualamountofareadivergenceobservedatthecriticalturningpoint.Alldimen-sionsarenormalizedbythehalfreactionthicknessoftheidealCJdetona-tion().ThelocationofreactioncompletionorthesonicsurfacecannotbedenedfortheidealCJdetonation.Thesonicsurfaceforthenite-sizechargewithareadivergence,however,canbedeterminedfromtheeigenvaluesolution.Notethattheareadivergencefromtheshocktothesonicplaneismoderate(30%increaseinarea)andthat,evenforthesmallestchargethick-nessthatcansupportdetonation,thethicknessoftheexplosiveslabisstillmorethanthreetimesthelengthofthedetonationfront(i.e.,thedistancefromtheshocktothesonicsurface).IncomparisontotheidealCJsolution,thelocationofthepeakinexothermicityandhalfreactionlengthhavemorethanquadrupledduetothelowerpost-shocktemperature,andtheexother-micityisstillniteasthesolutionpassesthroughsonic.Atthesonicsurface 88A.HigginsStewart[],andKleinetal.[].Theanalysisby[]and[]yieldsaresultforthecriticalvelocityidenticaltothatpreviouslyfoundbyZeldovichandKompaneetsfordetonationswithheatloss(2.38),reproducedherecrt DCJ11 21 \bEa (2.105)Theanalysisof[]producesaslightlymorecomplexexpressiondependentupon,whichnonethelessisequivalentto(2.105).ThisrelationisplottedinFig.2.18asadashedline.WhileexhibitingqualitativelysimilartrendstotheresultsobtainedbyintegratingthegoverningODEstondtheeigenvaluedetonationvelocity,quantitativeagreementisonlyfoundforveryhighvaluesofactivationenergy(wheretheasymptoticanalysisisintendedtoapply).2.6.5ComparisonstoExperimentExperimentswithcolumnsofdetonablegas(hydrogen/oxygen)connedbyinertgas(nitrogen)havebeenperformedby[].Somecharacter-isticimagesofsuccessfulpropagationandfailureofpropagationareshowninFig.2.19;furtherexperimentsarediscussedinChap.ofthisvolume.Theexpansionofthedetonationproductsandtheobliqueshockbeingdrivenintotheconninggasareclearlyvisible,asisthecurvatureoftheshockfront.Quantitativecomparisonofthemeasureddetonationvelocityinthesenite-diametercolumnsofdetonablegaswithZND-typecalculationusingtheNew-tonianmodelforinteractionwiththeconnement(aswasdoneinSect.2.6.4butwithamoredetailedchemistrymodel)wasdonebyTsugeetal.[andshowedgeneralagreementwiththeexperiments.Theexperimentaldata,however,hadrelativelylargeerrorbars,andmoreaccuratevelocitymeasure-mentswouldnecessitatemeasuringpropagationinlongercolumnsofdeton-ablegas,whichisadicultexperimenttoprepare. PropagationFailure bdbdacac Fig.2.19.Experimentalphotographsofdetonationsinnite-diameter,unconnedcolumnsofhydrogen/oxygen[ 2SteadyOne-DimensionalDetonations89PerhapsthemostimpressivedemonstrationlinkingtheZNDmodeltoanexperimentalresultisthestudyofgaseousdetonationsinporous-walledtubesandchannelsofRadulescu[].Duetotheowintotheporouswalls,thereactionzoneofthedetonationinsuchatubeorchannelexperiencesadiver-gentow,qualitativelysimilartothedivergenceresultingfromyieldingcon-nementorboundarylayersdiscussedearlierinthissection.Thisdivergenceresultsinvelocitydecitsand,forasucientlysmalltubediameter,failureofthedetonation.Theexperimentalmeasurementsofthevelocitydecitandfailurediameterinmixturesofhydrogen/oxygenandacetylene/oxygenwithlargeamountsofargondilutionexhibitedgoodcorrelationwithaZNDcalcu-lationwithdetailedchemistry(similartothatinSect.2.5)whichincludestheeectofowdivergence(asisdoneinthissection).Theradialowderiva-tive(or,equivalently,theareadivergence)wasestimatedbyassumingthattheowintotheporouswallwaschoked(sonic)attheporeopenings,withthenetoutowbeingscaledbytheporosityofthewall.Comparisonsofthismodeldemonstratedgoodagreementwiththeexperimentalresults,includingpredictionofthecriticaldiameteratwhichdetonationfailurewasobserved(seeFig.2.20).Whatismore,studiesinporous-walledtubesandporous-lined L*/dD/DCJ10-410-310-20.600.700.800.901.10 2H2 + O2ModelExp.C2H2 + 2.5O2 + 75%ArModelExp. Fig.2.20.Velocitydecitsobservedforgaseousdetonationspropagatinginporous-walledtubes,comparedtoaZNDmodelwithareadivergenceduetoowintothetubewalls.ThetubediameterisnormalizedbythecomputedreactionzonelengthoftheZNDdetonationwithdivergence,.Intheexperiments,initialpressurewaschangedinordertovaryreactionzonelengthwhilethetubediameterwasconstant[ 92A.Higginsnozzlethroat).Similartransoniccombustionregimesarebelievedtooccurinramaccelerators[].AdynamicalsystemsanalysisofthecriticalpointsinthesetypeofowswasrecentlyperformedbyDeSterck[Researcherswhohavelaboredtodeveloptheframeworkforunderstand-ingdetonationwavesshouldderivesatisfactionthattheireortsmayndawiderrangeofapplicationthanthenarroweldforwhichthatframeworkwasoriginallydeveloped.AcknowledgmentsThischapterwasdevelopedoutofdiscussionswithJimmyVerreault,OrenPetel,Fran¸cois-XavierJett´e,PatrickBatchelor,andDavidMack.VincentTanguaycontributedtotheanalysisoftheinclusionoftheworkdonebyfrictionindetonationsandtheTaylorwaveanalysisintheappendix.Jean-PhilippeDionnesdoctoraldissertationprovidedatemplateformuchofthischapter.JennyChaoandMateiRadulescuarethankedforsharingtheirexper-imentaldata.FanZhangandCraigTarverprovidedhelpfulandinsightfulcommentary.A.1AppendixA:GasdynamicsofDetonationProductsTheexistenceofsonicowattheexitplaneofadetonation,whichcomprisestheclassicalChapman Jouguetconditionanditsgeneralizationtononidealdetonations,meansthatthedetonationwaveisdecoupledfromtheexpansionofthedetonationproductsinthewakeofthewave.Thus,thedetailsoftheexpansiondonotneedtobeexplicitlyconsideredinsolvingforthedetonationwavepropertiesorstructure.Theexpansionofthegasthathasbeenprocessedbythedetonation(i.e.,theburnedgas)canbeofinterestinitsownrightforsomeapplications.Considerationofhowthedetonationexitstateismatchedwiththedownstreamexpansioncanalsoprovidesomeguidanceindeterminingthepossiblenon-CJexitstatesthatmightberealizable.ThegasdynamicsoftheunsteadyexpansionofdetonationproductswastreatedbyG.I.Taylorinaseminalwork[],andthesolutionhefoundisoftenreferredtoastheTaylorwave.Inthisappendix,theTaylorwaveoweldsolutionisbrieydevelopedusingthemethodofcharacteristicsfortheplanarcase(Sect.A.1.1matchingoftheTaylorwavewithdierentbranchesofdetonationsolutionsisthenexamined(Sect.A.1.2),andnallyamoreformalsimilaritysolutionforthecylindricalandsphericalcase(Sect.A.1.3)isdeveloped.A.1.1PlanarDetonationTaylorstreatmentofthedynamicsoftheproductsemergingfromapla-nardetonationbeginsbyassumingthatthedetonationwavepropagatesata 2SteadyOne-DimensionalDetonations93steadyspeed,withtheproductsleavingthewaveatconstantconditions.Itisfurtherassumedthattherearenoshockwavesintheowdownstreamofthedetonation.Thus,sincealltheoworiginatesatthesamestate(denotedstate2tobeconsistentwiththenotationinthischapter)andremainsisentropic,theentireowhasthesamevalueofentropy(i.e.,theowishomentropic).Thismeansthat,ateverypointintheow,characteristicwavesorig-inatingfromthedetonationbutpropagatingintheoppositedirectionasthewavehavethesamevalueoftheRiemanninvariant: 1c=u22 (2.106)wheretheprime()onisusedtodenotethatitisthevelocityintheunsteady,laboratory-xedreferenceframe,inordertodierentiateitfromthesteadyowvelocityusedthroughoutthischapter.From(2.106),itcanbeshownthatateverypointintheproducts,andarelinearlyrelated.Thisresultmeansthatcharacteristics(alongwhich constant)thatpropagateinthedetonationproductstowardthewavemusthaveconstantvaluesofandandarethereforestraightlinesinthe(x,tplane.Onepossiblesolutionthatcanbeconstructedwithstraightcharac-teristicsisacenteredrarefactionfanoriginatingattheorigin.Thedetonationisalsoassumedtooriginateattheoriginandhasnegligiblethicknesscom-paredtothedomainofinterest.Thus,theowpatternbecomesself-similar,asseeninFig.2.21.Atanypointinsidethecenteredrarefaction,thevalue x detonation wave + characteristics characteristics C+ = constantC = constant Fig.2.21.Centeredrarefactionsolutionfortheexpansionofproductsbehindadetonationwave,showingtheandcharacteristics 94A.Higginsmustequalthevalueof atthatpoint.Usingthisproperty,alongwiththeconstantcharacteristicsemanatingfromthedetonation,theowvelocityandsoundspeedcanbesolvedfor:x,t +1\bx tc2\t+1 (2.107)x,t +1\bx tu\t+2 (2.108)Notethatpositionandtimealwaysappearasthecombination ,verifyingthatthisisasimilaritysolution.Theotherthermodynamicproperties(pres-sure,density,temperature)canbedeterminedfromthesoundspeedbyusingtheisentropicrelations.ThevelocityprolebehindthewaveisplottedinFig.2.22.Forthisparticularplot,theconditionsatthedetonationexitplaneweretakenastheCJconditionsinthelimitoflargeheatrelease D=1 +1,limQc2 D= +1,limQ2 1=+1 ,limQp2 1D2=1 (2.109)whereavalueof2wasusedforFig.2.22.Notethatthevelocityinthecenteredrarefactionfangoestozeroandreversesdirection,reachinganescapespeedof -0.500.51 Fig.2.22.FloweldbehindaplanarCJdetonationwave(Taylorwave)showingpressureandowvelocityforbothclose-endedandopen-endedtubes( 96A.Higgins xtCJ detonation wave weak detonation wave u+c = Du+c DD strong detonation wave u+c DD strong detonation wave u+c = DCJ DetonationWeak DetonationStrong Detonation (supported)Strong Detonation decayingto CJ Detonationwallwallpiston at restpistonpistonpistonstops uniform region rarefactiondeceleratesdetonation x x x t t t dcba Fig.2.23.Expansionofcombustionproductsbehindadetonationwaveforthecasesof()CJdetonation,()weakdetonation,()strong(piston-supported)detonation,and()apiston-supporteddetonationinwhichthepistonstopsandtherarefactionsgeneratedovertakedetonation,deceleratingituntilthedetonationisparallelwithcharacteristics(CJdetonation)detonation,establishingaCJdetonation.Thissimplepicture,illustratedinFig.2.23d,perhapsprovidesamoresatisfyingexplanationforthelegitimacyoftheCJconditionofsonicowattheexitofanunsupporteddetonationwave.A.1.3CylindricalandSphericalDetonationsToconstructasolutionforthedynamicsoftheproductsbehindasphericaldetonationoriginatingfromapoint(oracylindricaldetonationinitiatedalongaline),theconservationofmassandmomentumforsphericalandcylindricalsymmetryareusedasfollows: 2SteadyOne-DimensionalDetonations99outthatinitiationofasphericaldetonationwillalwayslikelyrequiresomedegreeofinitialoverdrivethatwillresultinthedetonationbeinginitiallyonthestrongbranchofthesolution()andwillonlyasymptoticallyapproachanidealCJdetonationasthewaveexpands,sothattheissueoftheinnitegradientsinthesolutionisavoided[A.2AppendixB:CriticalSonicPointwithFrictionForadetonationwithfriction(andnoheattransfer),thecriticalconditionatwhichthewavepropagationvelocityequalsthevelocityofthecombustionproductscanbesolvedforanalyticallyasfollows[].Themomentumandenergyequations(2.27)and(2.28)canbeequated(excludingtheheatlossterm)viathefrictionfactor u1h+1 (2.117)andintegratedtoyield u1h+1 (2.118)whereisaconstantofintegrationthatcanbeevaluatedusingconditionsupstreamofthedetonationwave(,and).Atthecriticalsoniccondition,theowexitingthewaveissonicandequaltothevelocityoftheowapproachingthewave(inthelaboratory-xedframe,thisisequivalenttotheowthathasbeenprocessedbythewavebeingatrest),crs(2.119)wherethe2subscriptdesignatestheexitstate.Theconditionthatexitvelocityisthesameastheinowvelocitymeansthatthedensityisconstantacrossthewave().TheserelationsallowthecriticalMachnumberofpropagationtobesolvedforcrs c1= (2.120)Sincethedensityisconstantacrossthewave,thiscriticalsonicconditioncorrespondstoafrontofconstantvolumeexplosionpropagatingthroughthemediumwithapressureincreasegivenby p1=pCV (2.121)Atthiscriticalsoniccondition,theowvelocitybeingzerorelativetothewallattheexitofthewavemeansthatfrictionnolongerinuencestheow 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