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TheTunguskaAirburstRevisited:EvidenceforanIcy-Comet EquilibriumEvent HollisBlack Abstract The1908TunguskaexplosioninSiberiaremainsthelargestknownatmosphericimpactinrecorded history,yetnoimpactcraterordefinitivemeteoriteremnantshaveeverbeenfound.Thispaper advancesthehypothesisthattheTunguskaeventwasanicy-cometequilibriumdetonationa thermodynamicphasetransitioninwhichanincomingcometnucleusofpredominantlyvolatile materialunderwentflashvaporizationuponencounteringtheupperatmosphere.Theeventreacheda temporaryequilibriumbetweendrag-inducedheatingandexplosiveexpansion,producingascalding thermalwavethatflattenedtreeswithoutcombustion.Theresultingatmosphericvaporformeda high-altitudefoglayerconsistentwithnoctilucentcloudobservationsacrossEuropeinthedays followingtheblast. 1.Introduction TheTunguskaexplosiondevastatedmorethantwothousandsquarekilometersofforestnearthe PodkamennayaTunguskaRiveronJune30,1908.Witnessesreportedablindingflash,adouble shockwave,andanincandescentcolumnvisiblehundredsofkilometersaway.Yettheabsenceofa crater,scarcityofmeteoritefragments,andunusualburnpatternsremainunresolved.Conventional modelsasteroidalimpact,stonymeteoroidairburst,orsmallblackholeeachfailtoexplainthe combinationofhighradiantenergy,lowresidualheat,andchemicalsignaturesindicatingtransient volatiles.ThisworkreframesTunguskanotasanexplosionbutasanequilibriumeventamomentary stabilizationofthermodynamicextremes.Theobject,anicycometnucleus,disintegratedina self-limitingvaporizationcascade.Theatmosphereitselfmediatedtheenergyrelease,converting kineticenergyintodistributedlatentheatratherthancontinuouscombustion. 2.MethodsandFramework Thismodelassumesaninitialobjectmassbetween5×10^7and10^8kg,compositionallydominated bywatericewithtraceorganics.Entryangle˜30°,velocity˜27km/s.Atmosphericdragat8‒10km altituderaisedsurfacetemperaturebeyond2,000K,inducinginstantaneousphasetransitionofvolatiles intosuperheatedvapor.Atpeakheating,thesystemreachedanearbalancebetweenkineticdissipation andlatentenergyabsorptionametastableplateauwhereoutwardpressureequaledatmospheric confinement.Theresult:equilibriumdetonationaluminoussphereexpandingandcollapsingwithin milliseconds,releasingenergythroughrapidconvectionratherthandirectimpact. 3.ObservationalConstraints
Scaldingvs.Burning:Resinboiling,barkpeeling,andminimalcharringindicatescalding,not combustion.Tree-FallGeometry:Symmetricalflatteningaroundtheepicenterwithacentralstanding grove.AtmosphericOptics:NoctilucentcloudsacrossEuropesuggestamesosphericvaporplume. 4.Discussion TheTunguskaairburstlikelymarksthefirstobservedplanetary-scaleflashboil.Theforestwasnot burnedbutscaldedbyaradiativesteamenvelope.Theobjectsdisintegrationconvertedkinetic energyintoanexpandingwater-vaporshell,whichbrieflyreachedequilibriumwithsurroundingair pressurebeforedissipating.Thismetastablephaseanalogoustobreathfoggingoncold glassproducedaslow-dissipatingluminoushazeacrosstheNorthernHemisphere. 5.Conclusion TheTunguskaeventcanbedescribednotasanexplosionbutasanequilibriumbetweenheat,pressure, andatmosphere.Thescaldedtrees,fog-likeluminescence,andabsenceofcratercollectivelyindicatea transientbalancebetweenvaporexpansionandairresistanceanaturalthermodynamicexperimenton aplanetaryscale.TheTunguskaphenomenonthusrepresentsthefirstempiricallyrecordedexampleof ametastableatmosphericequilibriumreactioninnature. References 1.Chyba,C.F.,&Thomas,P.J.(1993).Impactdeliveryanderosionofplanetaryatmospheres. Science,262(5134),744‒747. 2.Boslough,M.B.,&Crawford,D.A.(2008).Low-altitudeairburstsandtheimpactthreat. InternationalJournalofImpactEngineering,35(12),1441‒1448. 3.Kuznetsov,D.etal.(2019).GeochemicalandmechanicalsignaturesoftheTunguskaexplosionarea. PlanetaryandSpaceScience,165,99‒109. 4.Black,H.(2025).Tunguska:IcyCometHypothesis(Updated).Zenodo.DOIpending.License:CC BY-NC4.0