Full metadata record
DC FieldValueLanguage
dc.contributor.authorAMME Marcusen_GB
dc.contributor.authorSVEDKAUSKAITE Jolantaen_GB
dc.contributor.authorBORS W.en_GB
dc.contributor.authorMURRAY FARTHING MAIREADen_GB
dc.contributor.authorMERINO J.en_GB
dc.date.accessioned2012-04-17T19:51:11Z-
dc.date.available2010-04-16en_GB
dc.date.available2012-04-17T19:51:11Z-
dc.date.created2010-03-01en_GB
dc.date.issued2007en_GB
dc.date.submitted2005-12-15en_GB
dc.identifier.citationRADIOCHIMICA ACTA vol. 95 no. 12 p. 683-692en_GB
dc.identifier.issn0033-8230en_GB
dc.identifier.urihttp://www.atypon-link.com/OLD/doi/abs/10.1524/ract.2007.95.12.683en_GB
dc.identifier.urihttp://publications.jrc.ec.europa.eu/repository/handle/JRC31810-
dc.description.abstractCurrent reactors spent nuclear UO2 fuel that will probably be directly disposed in geologic formations is assumed to get into contact with groundwater of a repository earliest after several thousands of years. After this time, its alpha activity will be still high enough to induce a process of water radiolysis that leads to production of oxidants and, probably, to the oxidative dissolution of the material, that would start a mobilisation of radiotoxic nuclides. The main oxidant produced during this process would be hydrogen peroxide (H2O2), which is thermodynamically unstable and can decompose during reactions with certain groundwater ions. Information on the stability of H2O2 is therefore important for assessing the behaviour of the material in the repository.en_GB
dc.description.sponsorshipJRC.E.3-Materials researchen_GB
dc.format.mediumPrinteden_GB
dc.languageENGen_GB
dc.publisherOLDENBOURG VERLAGen_GB
dc.relation.ispartofseriesJRC31810en_GB
dc.titleA Kinetic Study of UO2 Dissolution and H202 Stability in the Presence of Groundwater Ionsen_GB
dc.typeArticles in periodicals and booksen_GB
dc.identifier.doi10.1524/ract.2007.95.12.683en_GB
JRC Directorate:Nuclear Safety and Security

Files in This Item:
There are no files associated with this item.


Items in repository are protected by copyright, with all rights reserved, unless otherwise indicated.