The transfer of uranium isotopes U-234 and U-238 to the waters interacting with carbonates from Mendip Hills area (England)

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorUniv Reading
dc.date.accessioned2014-05-20T15:21:18Z
dc.date.available2014-05-20T15:21:18Z
dc.date.created2014-05-20T15:21:18Z
dc.date.issued2000-04-01
dc.identifierApplied Radiation and Isotopes. Oxford: Pergamon-Elsevier B.V., v. 52, n. 4, p. 965-983, 2000.
dc.identifier0969-8043
dc.identifierhttp://hdl.handle.net/11449/32463
dc.identifier10.1016/S0969-8043(99)00151-7
dc.identifierWOS:000086343900022
dc.identifier7430102726026121
dc.description.abstractLaboratory time-scale experiments were conducted on limestone and dolomite gravels from the Mendip Hills area, England, with the purpose of evaluating the release of U-238 and U-234 to different aqueous solutions. The U-234/U-238 activity ratio (AR) lab data were reliable to interpret the field data. The obtained values do not indicate a reduction in the amount of dissolved U and an increase in the AR of the remaining dissolved U as commonly observed for groundwater systems close to redox boundaries. (C) 2000 Elsevier B.V. Ltd. All rights reserved.
dc.languageeng
dc.publisherElsevier B.V.
dc.relationApplied Radiation and Isotopes
dc.relation1.123
dc.relation0,528
dc.rightsAcesso restrito
dc.sourceWeb of Science
dc.subjecturanium
dc.subjectisotopes
dc.subjectcarbonates
dc.subjectgroundwaters
dc.titleThe transfer of uranium isotopes U-234 and U-238 to the waters interacting with carbonates from Mendip Hills area (England)
dc.typeArtículos de revistas


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