hrr vs radius

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    AllofthefollowingdiscussionpertainstoaflamesheetmodelsolutionforacaseofaVgeometryflame

    stabilizedonacenterbodywithnoradius,withaconstantaxialvelocityandnoradialvelocityeffects.

    InmynotationIusethefollowingdefinitions:

    (1)

    and 1Firstconsiderthecaseinwhichthevelocityperturbationisacousticinnatureonly:

    (2) , Theoscillatingflamesurfaceposition()isgivenbythefollowingequation(comparetoPreetham,2008forVflameswhereK>0):

    (3)

    1

    Theheatreleaseisproportionaltotheflamesurfacearea. Onalocalbasiswecancalculatethe

    linearizedflamesurfacearea:

    (4)

    1

    Notethatforanaxisymmetriccase,thiswouldbesimilar,thedifferencebeingareadirectlyproportional

    totheradius. Observethatoneofthetermsinthesurfaceequationisnotafunctionofradius:

    (5)

    Takingthemagnitudeofthisgives:

    (6)

    || Thisisconstantwithrespecttoradius. Againrecallthatforanaxisymmetriccase,thedifferentialarea

    hasadifferentformandthus:

    (7)

    ||

    Bothhavethesamevalueforphaseangle,indicatingconvectionalongtheinclinedflamesurface:

    (8)

    Sotosummarize,theequationfortheflamesurfacepositionisthedifferenceoftwooscillatingterms,

    whoserelativephasedependsontheradialdistance,resultingininterferenceasafunctionofradius.

    However,intermsoftheamplitudeofoscillatingheatrelease,theamplitudehasaconstant(orlinear)

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    valueasafunctionofradius,similarlytotheamplitudeofoscillationsfortheconvectivedisturbance

    modelpresentedattheconference.

    Werewetodiscussvorticaldisturbancesinstead,theflamesurfacepositionsolutionis(againcompare

    toPreetham,2008):

    (9)

    1 1

    Inthiscasebothtermswillmakeacontributiontotheflamesurfacearea:

    (10) 1 1 1

    Ididnotdiscussthewaytodealwithmorecomplicatedexcitationconditionslikethisattheconference

    duetotimeconstraints,butthisisessentiallyhandledinaconvectivedisturbancemodelbyadding

    togethertheresponsetotwolinearlyindependentperturbationsmovingwithdifferentconvective

    speeds( and ). Indeedinthiscase,thecombinedsolutionWILLhaveanonconstant||becauseofinterferencebythetwodisturbances. However,lookingattheequation,wecanseethat

    whatshappeningiswehavetwoseparateperturbations,eachofwithhasconstantamplitudewith

    respecttoradius,butdifferentvaluesforthephaseangle. Thuswhenweaddthetwotogether,weget

    anonconstantvalue.