简介:Microplasmasareveryinterestingduetotheiruniquepropertiesandachievableregimesmaintainedatatmosphericpressures.Duetothesmallscales,numericalmodelingcouldcontributetotheunderstandingofunderlyingphenomenaasitprovidesaccesstolocalparameters—andcomplementsexperimentalglobalcharacteristics.Aself-consistentformalism,appliedtonanosecondpulsedatmosphericnon-equilibriumheliumplasmas,revealsthatseveralsuccessivedischargescanpersistasaresultofacombinedvolumeanddielectricsurfaceeffects.Thevaluableinsightsprovidedbythespatiotemporalsimulationresultsshowthecriticalimportanceofcoupledgasandplasmadynamics—namelygasheatingandelectricfieldreversals.
简介:JUNA(JinpingUndergroundlaboratoryforNuclearAstrophysics)isplaningtomeasurethe13C(α,n)16OandsomeotherimportantreactionsatorclosetostellarenergiesusingintenseheliumbeamoutofanECRdrivenacceleratorinJinpingUndergroundlaboratory[1].Deuteriumimpurityinionsourcewillproducessignificantamountofneutrons,limitingthebackgroundlevel.Tocontrolthedeteriumimpurity,wehavedevelopedamethodtomeasurethedeuteriumimpuritywithinHeliumbeamusingthed(d,p)treaction.
简介:Aone-dimensionalfluidmodelforhomogeneousatmosphericpressurebarrierdischargesinheliumispresentedbyconsiderilagelementaryprocessesofexcitationandionizationincludingametastableatomeffect.Usingthismodelweinvestigatethebehavioursoftheheliummetastableatomsindischargesaswellastheirinfluenceonthedischargecharacteristics.Itisshownthatthemetastableatomswitharelativelyhighconcentrationduringthedischargearemainlyproducedintheactivephaseofthedischargeanddissolvedintheoffphase.Itisalsofoundthatthemetastableatomcollisionscannotonlyprovideseedelectronsfordischargesbutalsoinfluencetheconcentrationofions.Areductionofmatestableatomdensityresultsinadropinthechargedparticledensitiesandcausesaqualitativechangeinthedischargepatterns.
简介:Theanisotropicpotentialdevelopedinourpreviousresearchandtheclose-couplingmethodareappliedtotheHBr-3He(4He,5He,6He,7He)system,andthepartialcrosssections(PCSs)attheincidentenergyof60meVarecalculated.Basedonthecalculations,theinfluencesoftheisotopeheliumatomonPCSsarediscussedindetail.TheresultsshowthattheexcitationPCSsconvergefasterthantheelasticPCSsforthecollisionenergyandthesystemsconsideredhere.AlsotheexcitationPCSsconvergemorerapidlyforthehigh-excitedstates.Thetaileffectispresentonlyinelasticscatteringandlow-excitedstatesbutnotinhigh-excitedstates.Withtheincreaseofreducedmassofthecollisionsystem,theconvergingspeedoftheelasticandexcitationPCSsslowsdown,andthetaileffectgoesup.
简介:Hydrodynamicpropertiesandstructureofstrongshockwavesinclassicaldenseheliumaresimulatedusingnon-equilibriummoleculardynamicsmethods.Theshockspeedinthesimulationreaches100km/sandtheMachnumberisover250,whichareclosetotheparametersofshockwavesintheimplosionprocessofinertialconfinementfusion.Thesimulationsshowthatthehigh-Mach-numbershockwavesindensemediahavenotabledifferencesfromweakshockwavesorthoseindilutegases.Theseresultswillprovideusefulinformationontheimplosionprocess,especiallythestructureofstrongshockwavefront,whichremainsanopenquestioninhydrodynamicsimulations.
简介:Inthispaper,theobtainedexperimentalresultsconcerningcreationofbulkelementaryexcitations(BEEs)iniso-topicallypureliquid4Heatlowtemperatures~60mKarediscussed.Positiverotons’(R+-rotons)creationbyapulsedheaterwasstudied.Signalswererecordedforthefollowingquantumprocesses:quantumevaporationof4He-atomsfromthefreeliq-uid-heliumsurfacebytheBEEsoftheliquidhelium-II,andBEEsreflectionfromthefreesurfacebackintothebulkliquid.Typicalsignalsareshown,andratiosofsignalamplitudesareevaluated.Forlongheaterpulsesfrom5to10μs,appearanceofthesecondatomiccloudconsistingofevaporated4He-atomswasobservedinadditiontothefirstatomiccloud.Itisthoughtthatthefirstatomiccloudoftheevaporatedheliumatomsconsistsofveryfast4He-atomswithenergies~35Kevaporatedbypositiverotonswiththespecialenergies~17K(~2ER~2×8.6KwithERrepresentingtherotonminimumenergy)correspondingtothethirdnon-dispersiveZakharenkowave.Thesecondcloudofslower4He-atomswascreatedbysurfaceelementaryexcitations(SEEsorripplons)possessingthespecialenergies~7.15Krepresentingthebindingenergy.ItwasassumedthatsuchSEEscanbecreatedbyphononsincomingtotheliquidsurfacewithspecialenergies~6.2Kcorrespondingtothefirstnon-dispersiveZakharenkowave,whichcaninteractattheliquidsurfacewiththesamephononsalreadyreflectedfromthesurfaceforlongheaterpulses.Also,somepulsed-heatercharacteristicswerestudiedinordertobetterunderstandthefeaturesofsuchheatersinlowtemperatureexperi-ments.
简介:Wereportontheexperimentalobservationoftheairflowmotioninducedbyan800nm,1kHzfemtosecondfilamentinacloudchamberfilledwithairandhelium.Itisfoundthatvortexpairswithoppositerotationdirectionsalwaysformbothbelowandabovethefilaments.WedonotobservethatthevorticesclearlyformedabovethefilamentinairjustbecauseoftheformationofsmallerparticleswithweakerMiescattering.Simulationsoftheairflowmotioninheliumareconductedbyusingthelaserfilamentasaheatsource,andthesimulatedpatternofvorticesandairflowvelocityagreewellwiththeexperimentalresults.更多还原
简介:TheRichtmyer–Meshkovinstabilityofa‘V'shapedair/heliumgaseousinterfacesubjectedtoaweakshockwaveisexperimentallystudied.Asoapfilmtechniqueisadoptedtocreatea‘V'shapedinterfacewithaccurateinitialconditions.Fivekindsof‘V'shapedinterfaceswithdifferentvertexanglesareformedtohighlighttheeffectsofinitialconditionsontheflowcharacteristics.Theresultsshowthataspikeisgeneratedaftertheshockimpact,andgrowsconstantlywithtime.Asthevertexangleincreases,vorticesgeneratedontheinterfacebecomelessnoticeable,andthespikedevelopslesspronouncedly.Thelineargrowthrateofinterfacewidthaftercompressionphaseisestimatedbyalinearmodelandarevisedlinearmodel,andthelatterisproventobemoreeffectivefortheinterfacewithhighinitialamplitudes.Thelineargrowthrateofinterfacewidthis,forthefirsttimeinaheavy/lightinterfaceconfiguration,foundtobeanon-monotonousfunctionoftheinitialperturbationamplitude–wavelengthratio.
简介:在主要Yishui-Tangtou差错的脚墙的花岗石的碎裂岩withmylontization招待的Longquanzhan金矿床。在液包体的~3He/~4He比率从0。14~0。24R/Ra,近到那些,外壳来源helium.~(40),Ar/~(36)Ar比率被测量是289-1811,比那些稍微高大气的氩。氦和氩同位素的分析的结果建议形成矿石的液体从外壳主要被导出。δ~(18)O每千每千从静脉石英范围from-1.78液包体珍视到4.07,并且δD液包体珍视在-74per之间变化千并且-77每千。氢和氧同位素数据显示了为Longquanzhan金矿床的液体在矿化作用的过程与天落水混合了的那形成theore。这与从氦和氩同位素数据的结论一致。