dc.contributor.author | Baker, Robert | en |
dc.contributor.author | Mc Kenna, Cora | en |
dc.date.accessioned | 2017-01-12T12:44:43Z | |
dc.date.available | 2017-01-12T12:44:43Z | |
dc.date.issued | 2016 | en |
dc.date.submitted | 2016 | en |
dc.identifier.citation | S. 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 - 6393 | en |
dc.identifier.other | Y | en |
dc.description | PUBLISHED | en |
dc.description.abstract | The 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 ion | en |
dc.description.sponsorship | We 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.extent | 6383 | en |
dc.format.extent | 6393 | en |
dc.language.iso | en | en |
dc.relation.ispartofseries | Dalton Transactions | en |
dc.relation.ispartofseries | 45 | en |
dc.rights | Y | en |
dc.subject | uranyl minerals | en |
dc.subject.lcsh | uranyl minerals | en |
dc.title | An investigation of the interactions of Eu3+ and Am3+ with uranyl minerals: implications for the storage of spent nuclear fuel. | en |
dc.type | Journal Article | en |
dc.type.supercollection | scholarly_publications | en |
dc.type.supercollection | refereed_publications | en |
dc.identifier.peoplefinderurl | http://people.tcd.ie/bakerrj | en |
dc.identifier.peoplefinderurl | http://people.tcd.ie/mckennc6 | en |
dc.identifier.rssinternalid | 122820 | en |
dc.identifier.doi | http://dx.doi.org/10.1039/C6DT00199H | en |
dc.rights.ecaccessrights | openAccess | |
dc.identifier.rssuri | http://pubs.rsc.org/en/content/articlelanding/2014/dt/c6dt00199h#!divAbstract | en |
dc.identifier.orcid_id | 0000-0003-1416-8659 | en |
dc.contributor.sponsor | Irish Research Council (IRC) | en |
dc.identifier.uri | http://hdl.handle.net/2262/78696 | |