searchthissite AirFilterAlphaSpectrometryReport AirFilterAlphaSpectrometryReport Navigation Posted:7/31/201121:05 LatestNews BacktoMainUCBAirandWaterSamplingPage RealtimeAir Monitoring BacktoAirSamplingResultsPage Environmental Monitoring AboutRadWatch BRAWMData (2011-2013) Summary BRAWMtookanairfiltersampleinmid-Aprilandperformedalphaspectrometryontheairfilter.We didnotdetectanyUranium,Plutonium,orAmericium-241,andourcalculateddetectionlimitsindicate safelevels.OurlimitsaremuchhigherthanthelimitssetbytheEPAintheirtestingforUraniumand Plutonium.Ifyouwouldliketoskipdirectlytoourlimits,pleaseclickhere. KelpWatch Introduction FrequentlyAsked Questions/AskA Question Radioactivitycomesinthreeprimaryforms:alpha,beta,andgammadecay.Aradioactivenucleuswill undergooneormoreofthesedecays,releasingparticleswithcharacteristicenergies. Contact WhoWeAre Trending Donate! ThefissionproductnucleithatarethesubjectofBRAWM'smeasurementsarebetaemitterswith associatedgammarays.Betaparticlesarehighenergyelectronsthatdonothavediscreteenergies —theyarereleasedinacontinuumwithan"endpoint"energythatdependsonthenucleus.Gamma raysarephotons("particlesoflight")andhavediscreteenergies.Thesediscreteenergiesare fingerprintsforaspecificnucleus,anddetectinggamma-raysiswhatBRAWMspecializesin.For example,Cesium-137hasastronggamma-ray"line"at662keV,andthatiswhatwelookforinour spectra. Whataboutalphadecay?Alphaparticlesareheliumnuclei(twoprotonsandtwoneutrons),andthey areverysimilartogammaraysinthattheyarereleasedatspecificenergiesthatarefingerprintsofa givennucleus.Forexample,Uranium-238hastwostrongalphalinesat4.151and4.198MeV.Since manynucleimightbealphaemittersbutnotstronggammaemitters(e.g.,U-238andPu-239),one mustuseanalphadetectortodetectthem. Alphaspectroscopyisdifficult,evenwhencomparedtogammaspectroscopy.Theprimarydifference isthatsincealphaparticleshaveelectriccharge(+2),eventinyamountsofmaterialbetweenthe nucleusandthedetectorwillcauseenergylossorcompletestoppingofthealphaparticle.Soinstead ofnice,discretelinesyouwillfindsmearedoutblobsinyourspectrum—orevennothingatall.The morethealphalinesaresmearedandblocked,theworseyourabilitytodetectandidentifyalpha emittersis.Gamma-raysdonotsufferfromthisproblem. ExperimentalSetup Weplacedapieceoffilterpaper(3MFiltrete)overthenozzleoftheshopvacusedforourair measurementsforthreedays,April16–19,2011.Wefilteredatotalofapproximately5,500,000liters ofair(5,500cubicmeters).Attheendofthecollectiontime,thefilterpaperhadturnedblackfromthe airparticlesitfilteredfromtheair. Withinminutes,wetookthefilterpaperandplaceditinfrontofandnearlyincontactwithasiliconPIN alphadetector.Thedetectorandsamplewerehousedinasealedchamberthatweevacuatedsothat theairwouldnotblockthealphaparticles.Thechamberwascoveredwithanopaqueblackclothso thattheambientlightintheroomwouldnotcreatenoiseinthesilicondetector. NaturalAlphaBackgroundfromRadondecayproducts Withinminutes,therewerefourprominentalphalinesbetween5and9MeV.Weidentifiedtheseas comingfromPolonium-210(5.3MeV),Polonium-212(8.8MeV),Polonium-214(7.7MeV),and Bismuth-212(6.1MeV),allnaturally-occurringisotopesthataredecayproductsofRadongas (specifically,thetwoisotopesRn-222andRn-220).Itisnotsurprisingtoseethem.Polonium-214was thebrightestline,butitwasonlyvisibleinthespectrumduringthefirstfewhours.Thisiseasily explainedbyitspositioninthedecaychainofRadon-222—itis"fed"bythedecaysofthebetaemittingnuclidesLead-214(27minutes)andBismuth-214(20minutes),andithasanextremelyshort half-lifeitself(164microseconds).SoPo-214isverybrightforthefirsthourbutdisappearswhenthe decaychainisexhausted. Thisplotshowsthespectrumfromthefirstthreehours,overlaidwithaspectralmodelforthefour isotopes: Thisnextplotshowsthespectrumfor3daysafterthePo-214hasdecayedaway.Thethreeisotopes Po-210,Bi-212,andPo-212remain: Afterthefirst3days,theBi-212andPo-212entirelydisappear.Thismakessensebecausetheyare ontheRn-220decaychainafterthebeta-emittingisotopeLead-212(10.6hours),soafterafewhalflivesofPb-212thisdecaychainisexhausted. WhatremainsisPolonium-210(138days),whichis"fed"byanotherRadondecayproduct,Lead-210 (22.3years).SoPo-210remainsforaverylongtime.Infact,itsactivityhasbeensteadilyincreasing duringourtestasmoreandmorePb-210decaysintoPo-210.Hereiswhatthespectrumlookslike fromthreedaysafterthestartuntilpresently: SearchingforUraniumandPlutoniumSignatures Plutonium,Uranium,andAmericiumisotopesemitalphaparticlesatwell-knownenergies,allinthe vicinityofthe5.3MeVlinefromPo-210: Isotope AlphaEnergies U-238 4.1–4.2MeV U-234 4.7–4.8MeV U-235 4.3–4.4MeV Pu-238 5.4–5.5MeV Pu-239 5.1–5.2MeV Am-241 5.4–5.5MeV Sothebasicideaistolookatthealphaspectrumatthoselocationsandseeifthereisanyexcess fromthoseisotopes.Aline,ifpresent,shouldhavethesameshapeasthealphalinesfromthe naturally-occurringisotopes—i.e.,"triangle"shapeswiththerightmostedgeatthealphalineenergy. IfitthePo-210spectrumwithamodel(redlineinthepreviousfigure),andsubtractedthemodelfrom theobservedspectrum.Itisinthissubtractedspectrumthatthesignaturesoftheisotopesofinterest wouldlurk.Hereisthesubtractedspectrum,withblacklinesdenotingthe"1sigma"uncertaintiesfor eachbin: Thesubtractedspectrumhasnoclearsignaturesofanyexcesscounts.Thesedataappeartobe randomfluctuationsaroundzero.Sonowwemustgoaboutdeterminingwhatthedetectionlimit (MDA)ofthistestis. CalculatingtheLimits Toinferwhatthisnon-detectionmeans,wecalculatedanupperlimitonthetotalactivityconcentration fortheseisotopes. Oneveryimportantconceptisefficiency.Efficiencyisthefractionofallemittedalphaparticlesthatare detectedbythedetector.Therearevariousindependentcomponentstoit,whichIhave conservativelyestimatedasfollows: Efficiency Estimate Reasoning Geometric 3.9% Thisistheratiooftheareaofthedetectortotheareaofthefilterpaper. Left/Right 50% Halfofallalphaswilltravelawayfromthedetector,andhalfwilltravel towardsit. Escape fromfilter 0.33% Thisiswherethelargestuncertaintylies.Thiswasestimatedbyassuming a1micronrangeforalphaparticlesinorganicmaterial,andnotingthatthe totalthicknessofthefilterpaperis150microns,withacoursemesh coveringabout50%ofthefinefilterpaper. Detection 100% Essentiallyallalphasthatstrikethedetectorshouldbedetected. Total 0.0064% SimilartotheefficiencyiswhatIwillcallthe"spectralformfactor."Tocalculatethedetectionlimits, we'llselectacertainregionofthespectrum,suchas3.2–4.2MeVforU-238.Sinceanalphalinewill spreadoutbeyondthisrange,weneedtoknowwhatfractionshouldfallinthatselectedrange.Based onthePo-210lineshape,awindow1MeVwideshouldyieldgoodsensitivity,butonlyabout50%of countswouldberegistered.Wewilluse1MeVwindowsandaspectralformfactorof50%. Hereissomemathshowinghowminimumdetectableactivity(MDA)iscalculated: ActivityConcentration(Bq/L) ×AirVolume(L) Numberof Alphasfrom Source = ×CountingTime(sec) ×Efficiency(%) ×Spectralformfactor(%) NumberofAlphasfromSource Activity Concentration (Bq/L) = Background Noise = Minimum Detectable Activity(Bq/L) AirVolume(L)×CountingTime(sec)×Efficiency(%)×Spectralform factor(%) SquareRoot[NumberofAlphasinBackground] 2×BackgroundNoise ≈ AirVolume(L)×CountingTime(sec)×Efficiency(%)×Spectralform factor(%) Forourtest,herearetherelevantdata: AirVolume: 5,500,000L CountingTime: 7,259,912sec Efficiency: 0.0064%(estimated) HereareourestimatedMinimumDetectableActivitiesforeachisotopeofinterest: Isotope Rangeof spectrum investigated Numberof alphasin background MDA(Bq/L) MDA(aCi/m3) Yearsof breathingthe airtoequal dosefrom oneplane flight(5 millirem) U-238 3.2–4.2MeV 3,036 <8.6E-8Bq/L <2,300aCi/m 3 >2.6years U-234 3.8–4.8MeV 4,354 <1.0E-7Bq/L <2,800aCi/m 3 >1.9years U-235 3.4–4.4MeV 3,445 <9.2E-8Bq/L <2,500aCi/m 3 >2.4years Pu-238 4.5–5.5MeV 5,047 <1.1E-7Bq/L <3,000aCi/m 3 >0.7years Pu-239 4.2–5.2MeV 5,588 <1.2E-7Bq/L <3,200aCi/m 3 >0.6years Am-241 4.5–5.5MeV 5,047 <1.1E-7Bq/L <3,000aCi/m 3 >0.7years ComparisonwithEPAresults WhileourlimitsarecomparabletothelimitswehavesetforfissionproductisotopesfromJapan,the EPAreachedmuchlowerlimits.TheEPAperformedseveraltestsforPuandUinthefirstfewweeks aftertheFukushimadisaster.Theyissuedareportontheirfindings.InSanFrancisco,therewasa detectionofU-238,butnodetectionsofU-234,U-235,Pu-238,orPu-239.Herearethedata, accessedviatheEPAquerysearch.MDAwasestimatedbytakingtwicetheuncertainty(CSU): Isotope Result (aCi/m3) MDA(aCi/m3) U-238 14.1±6.3 12.6 U-234 ND 10.8 U-235 ND 8.8 Pu-238 ND 7.0 Pu-239 ND 11.6 Soourlimitsareabout200–300timeshigherthantheEPAlimits.Eventhoughwespentalongertime collectingdata,thesignal-to-noiseisjusttoopoorforustoreachsimilarlimits. Becauseofthedifficultiesinherentinmeasuringalphaparticlesfromanairfilter,thestandard procedureistoperformsomechemistryonthefiltertoextractandconcentratetheactinides (Uranium,Plutonium,Americium,andothers).Theseelementsarethenelectroplatedontoametalfilm andplacedinfrontofadetector.Becausethereisnointerveningfiltermaterial,thesesampleshave muchsharperlinesandgreatersensitivity(i.e.,lowerlimits)canbeachieved. Sinceuraniumandplutoniumhavelonghalf-lives,wemayconsiderperformingotheranalysesonour filtersamplethatcouldbemoresensitive. MoreInformation Ifyouwouldliketoknowmoreaboutalphaspectroscopy,hereareafewonlinereferences: EPAAlphaSpectrometryTutorial Canberra:APracticalGuidetoSuccessfulAlphaSpectroscopy Canberra:SamplePreparationforAlphaSpectroscopy FeelfreetoDonate,Contactus,orAskaQuestion PoweredbyDrupal
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