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dc.contributor.authorHood, Darden
dc.contributor.authorHatfield, Ronald
dc.contributor.authorPatrick, Christopher
dc.contributor.authorStipp, Jerry
dc.contributor.authorTamers, Murry
dc.contributor.authorLeidl, Robert
dc.contributor.authorLyons, Barbara
dc.contributor.authorPolach, Henry
dc.contributor.authorRobertson, Steve
dc.contributor.authorZhou, Weijian
dc.date.accessioned2021-02-11T20:15:23Z
dc.date.available2021-02-11T20:15:23Z
dc.date.issued1989-01-01
dc.identifier.citationHood, D., Hatfield, R., Patrick, C., Stipp, J., Tamers, M., Leidl, R., ... & Zhou, W. (1989). Radon elimination during benzene preparation for radiocarbon dating by liquid scintillation spectrometry. Radiocarbon, 31(3), 254-259.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200011760
dc.identifier.urihttp://hdl.handle.net/10150/653103
dc.descriptionFrom the 13th International Radiocarbon Conference held in Dubrovnik, Yugoslavia, June 20-25, 1988.
dc.description.abstractRadon gas is a serious contaminant in radiocarbon dating by radiometry. The low specific ionizations associated with the a-particle emitting radon and its Beta-particle emitting daughters overlap within the 14C counting window. Elimination of radon is therefore imperative for precise 14C age determinations. This paper deals with the sources and mechanism of incorporation of radon affecting 14C dating by liquid scintillation (LS) counting, and reviews conventional radon elimination practices in 14C laboratories. It demonstrates, based on rigorous multichannel and multiparameter alphaand Beta-particle spectral analyses of some 1000 benzene samples, that parent radium is not present and that its daughter radon is quantitatively eliminated during dynamic vacuum recovery of benzene at -78 degrees C. However, the radon-free benzene can be recontaminated by exposure to air containing traces of radon, such as is common in concrete or low-lying laboratories. The use of radon-free air, when exposing the benzene to the atmosphere, and the monitoring of radon counts from the environment and sample benzene in a fixed 'radon window', are essential prerequisites to the quality control of 14C age determinations in very low background systems.
dc.language.isoen
dc.publisherDepartment of Geosciences, The University of Arizona
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectradon
dc.subjectnoble gases
dc.subjectaromatic hydrocarbons
dc.subjectbenzene
dc.subjecthydrocarbons
dc.subjectliquid scintillation methods
dc.subjecttechniques
dc.subjectorganic compounds
dc.subjectorganic materials
dc.subjectsample preparation
dc.subjectmethods
dc.subjectC 14
dc.subjectcarbon
dc.subjectisotopes
dc.subjectradioactive isotopes
dc.subjectabsolute age
dc.titleRadon Elimination During Benzene Preparation for Radiocarbon Dating by Liquid Scintillation Spectrometry
dc.typeProceedings
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.noteThis material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries.
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume31
dc.source.issue3
dc.source.beginpage254
dc.source.endpage259
refterms.dateFOA2021-02-11T20:15:23Z


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