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   吋ぜ
AkihikoIto OitaUniversity
TadashiKonishi OitaUniversity
ABSTRACT Werecentlydevelopedtwodiferentopticaltechniquesinorder
to.simu1taneously measure transient.2・D profiles of'velocity, temperature and fuel concentration that were generated by a spreadingflameoverliquidfuels. Onetechniqueemploysaparticle- tracksystemcombinedwithalaser-shetsystem(PTLS)andahigh sp回 dcamera,whiletheothertechniqueemploysadualwavelength holographicinterferometry(DWHI). 官lep1工S systemrevealed transient2・D]?rofilesofflameinducedflow,whileDWHIrevealed 2-Dprofilesoffuelconcentrationoverliquids. Inthispaperwe presentaseriesofvelocityprofi1esforapulsatingflamespreaqover propanolandconcentrationprofi1esforgaseouspropanoldeteロnined withP1LSandDWHIrespectively.Othetresearchershavepred.icted theformationofsma1twincirculations,oneagas-phasecirculation
justaheadoftheflame'sleadingedge,andtheotherasmalliquid circulationjustunderneaththegas-phasecirculation. OurPTLS results confirmed'these predictions,.ie.,the formation of5・10 milimeterdiametercirculatiQninthegasphaseandanacompanying aproximately20milimeterdiameterliquidcirculation. Basedon these data,we ofer a phenomenologica1 expl加 ation of the mechanismofpulsatingflamespread. Inadition,weshowthat DWHIisaverypromisingtechniqueformeasurlngtr佃 sient釦el- concen釘ationprofilesoverliquids.
INTRODUCTION HistoricalBackaround
百lephenomenonofflamespreadoverliquidsisofc沼 町 四t interestbecauseofitsimportanceωfiresafety. Ourobj巴ctiveis diferen.tWewishtolearnmoreaboutthefundamenta1mechanism oftheflamespread. Anexcel1entreviewoftheliteratureonthis problem was published by Ros s [19 94] and Hirano and Suzuki [193]andthetheoretiCa1backgroundoftheproblemwasprovided byWiliams[1985]. 官leyadresedmanyoftheproblemsthat nededto'beinvestigated.
百lepresentpaperisacontinuationofourpreviousstudieson flamespreadoverliquids[Ito,Masuda,Saito,191;Ito,Saito,叩d Cremers,195;'andTashtoush,Narumi,Ito,Saito,andCremers, 196].Inぬeses旬diesweapliedholographicinterferometry(HI)旬 obtainadetailedandinstantaneoustemperaturedistributioninthe
HTD.Vol.352,ProceedingsoftheASMEHoatTransferDivision Volume2 ASME1997
THEMEASUREMENTOFTRANSIENT2・DPROFILESOF VELOCITVANDFUELCONCENTRATIONOVERUQUIDS
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141
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AkiraNarumi KanagawaInstituteofTechnologγ
GassanTashtoush,KozoSaito, andClifordJ.Cremers UniversityofKentucky
liquidphasene紅 白efueIsurface. Ineachofmethanol,ethanoIand propanolwefoundsubsurface-liqu~d conv即位oninboththeuniform spread,andpuIsatingspreadregions.Tounderstandthemechanisms offlamespreadinbothr~gions, researcherstriedtoidenti勿 印 刷uor heat-transferprocesbetwentheflame'sIeadingedgeandtheliquid, whetheritocursthroughthegasphase"liquidph出 eorboth.When theliquiqconvectionisproducedandittravelsaheadoftheflame's leading'edge,theflamespreadislikelytobecontroledbyitbecause the convection car ries the high temperaωre liquid ahead of the flame'sleading凶ge. This.enhancesevaporationofliquidvapor resultingintheformationofaflamablemixtureoffuelandair throughwhichtheflamecanspread. Ifthereisnoliquidconvection aheadofthefl仰 向 1eadingedge,themajorheattransferCalocur
betwertheflame'sleadingedgeandtheliquidbyc<;mductionand radiationinthegasphase,becauseconductionthroughtheliquidis negligible[GlasmanandDryer,1981].
Liquidconvectionisuniquetoflamespreadoverliquidsandit complicatesthespreadingprocesincomparisontoflamespread oversolids,whichhavenocondensedphaseconvection[Wiliams, 1985]. 古川s,itisimportanttQmeasuretempera加reandvelocity profilesintheliquidphase. Akita[1972]wasthefirstresearcherto aplyashadowgraphtechniquetovisua1izetheliquidconvection. Hereportedthe.formationofliquidconvectioriinthepulsating region,butnoliquidconvectionintheuniformspreadregion.Based on Akita's data,Glas sman and Dryer [1981] proposed that the uniformspreadiscontroledbyheatconductionth:roughthegas
phase,whiIeinthepulsatingregiontheliquidconvectionplaysan importantrole. However,theproposedIl).echanismfortheuniform spreadisquestionable,b巴causethegas-phaseconductionmaynot transfersuficientheatfortheflametospreadatarateofnearly10 cmls.
To, solve this problem買 we developed 佃 HI system and performedthetr釦 sientmeasurementofliquidtemperaωre[Ito, Masuda,andSaito,'191]. 百leresponsetimeofourHIsystemis les s than 1 micro second. W e estimate the uncertainty of the spatia1 resolution to be ま 0.1 m m,and the tempera加 re resolution to be 土 0.1 oc[lto,Masuda,andSaito,191]. Usingthemsystem,we observedalargeliquidconvectionbothintheuniformandpuIsating spreadregions. TheiIquidconvectionintheuniformspreadr,
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