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dc.contributor.authorBaker, Roberten
dc.contributor.authorMc Kenna, Coraen
dc.date.accessioned2017-01-12T12:44:43Z
dc.date.available2017-01-12T12:44:43Z
dc.date.issued2016en
dc.date.submitted2016en
dc.identifier.citationS. Biswas, R. Steudner, M. Schmidt, C. McKenna, L. L. Vintro, B. Twamley and R.J. Baker, An investigation of the interactions of Eu3+ and Am3+ with uranyl minerals: implications for the storage of spent nuclear fuel., Dalton Transactions, 45, 2016, 6383 - 6393en
dc.identifier.otherYen
dc.descriptionPUBLISHEDen
dc.description.abstractThe reaction of a number of uranyl minerals of the (oxy)hydroxide, phosphate and carbonate types with Eu( III ), as a surrogate for Am( III ), have been investigated. A photoluminescence study shows that Eu( III ) can interact with the uranyl minerals Ca[(UO 2 ) 6 (O) 4 (OH) 6 ]·8H 2 O (becquerelite) and A[UO 2 (CO 3 ) 3 ]· x H 2 O (A/ x =K 3 Na/1, grimselite; CaNa 2 /6, andersonite; and Ca 2 /11, liebigite). For the minerals [(UO 2 ) 8 (O) 2 (OH) 12 ]·12H 2 O (schoepite), K 2 [(UO 2 ) 6 (O) 4 (OH) 6 ]·7H 2 O (compreignacite), A[(UO 2 ) 2 (PO 4 ) 2 ]·8H 2 O (A = Ca, meta -autunite; Cu, meta -torbernite) and Cu[(UO 2 ) 2 (SiO 3 OH) 2 ]·6H 2 O (cuprosklodowskite) no Eu( III ) emission was observed, indicating no incorporation into, or sorption onto the structure. In the examples with Eu 3+ incorporation, sensitized emission is seen and the lifetimes, hydration numbers and quantum yields have been determined. Time Resolved Laser Induced Fluroescence Spectroscpoy (TRLFS) at 10 K have also been measured and the resolution enhancements at these temperatures allow further information to be derived on the sites of Eu( III ) incorporation. Infrared and Raman spectra are recorded, and SEM analysis show signi fi cant morphology changes and the substitution of particularly Ca 2+ by Eu 3+ ions. Therefore, Eu 3+ can substitute Ca 2+ in the interlayers of becquerelite and liebigite and in the struc- ture of andersonite, whilst in grimselite only sodium is exchanged. These results have guided an investi- gation into the reactions with 241 Am on a tracer scale and results from gamma-spectrometry show that becquerelite, andersonite, grimselite, liebigite and compreignacite can include americium in the structure. Shifts in the U v O and C – O Raman active bands are similar to that observed in the Eu( III ) analogues and Am( III ) photoluminescence measurements are also reported on these phases; the Am 3+ ion quenches the emission from the uranyl ionen
dc.description.sponsorshipWe thank Irish Research Council for funding this work via a Government of Ireland Postdoctoral Fellowship (SB), Prof. Balz S. Kamber from the Department of Geology at TCD for assist- ance with ICP-MS measurements and the Centre for Microscopy and Analysis at TCD for the SEM and EDX measurements. This work was co-financed (M. S.) by the Helmholtz Gemeinschaft Deutscher Forschungszentren (VH-NG-942) and (R. S.) from the Federal Ministry of Education and Research (BMBF) under grant 02NUK019D.en
dc.format.extent6383en
dc.format.extent6393en
dc.language.isoenen
dc.relation.ispartofseriesDalton Transactionsen
dc.relation.ispartofseries45en
dc.rightsYen
dc.subjecturanyl mineralsen
dc.subject.lcshuranyl mineralsen
dc.titleAn investigation of the interactions of Eu3+ and Am3+ with uranyl minerals: implications for the storage of spent nuclear fuel.en
dc.typeJournal Articleen
dc.type.supercollectionscholarly_publicationsen
dc.type.supercollectionrefereed_publicationsen
dc.identifier.peoplefinderurlhttp://people.tcd.ie/bakerrjen
dc.identifier.peoplefinderurlhttp://people.tcd.ie/mckennc6en
dc.identifier.rssinternalid122820en
dc.identifier.doihttp://dx.doi.org/10.1039/C6DT00199Hen
dc.rights.ecaccessrightsopenAccess
dc.identifier.rssurihttp://pubs.rsc.org/en/content/articlelanding/2014/dt/c6dt00199h#!divAbstracten
dc.identifier.orcid_id0000-0003-1416-8659en
dc.contributor.sponsorIrish Research Council (IRC)en
dc.identifier.urihttp://hdl.handle.net/2262/78696


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