001     1016755
005     20240708133945.0
037 _ _ |a FZJ-2023-03741
041 _ _ |a English
100 1 _ |a Brandt, Felix
|0 P:(DE-Juel1)144040
|b 0
|e Corresponding author
|u fzj
111 2 _ |a 21st Jena Remediation Symposium
|c Jena
|d 2023-10-04 - 2023-10-06
|w Germany
245 _ _ |a Retention Mechanisms for 226Ra: solid-solution formation and adsorption
260 _ _ |c 2023
336 7 _ |a Conference Paper
|0 33
|2 EndNote
336 7 _ |a Other
|2 DataCite
336 7 _ |a INPROCEEDINGS
|2 BibTeX
336 7 _ |a LECTURE_SPEECH
|2 ORCID
336 7 _ |a Talk (non-conference)
|b talk
|m talk
|0 PUB:(DE-HGF)31
|s 1696850902_26498
|2 PUB:(DE-HGF)
|x Invited
336 7 _ |a Other
|2 DINI
520 _ _ |a The fate of Ra, a decay product of 232Th, 235U, and 238U, in the environment is relevant because Ra is an important source of radioactivity in technically enhanced naturally occurring radioactive materials (TENORM). Ra-containing TENORM essentially originates from mining (e.g., uranium, phosphate) and milling operations, from coal ash, and raw material production processes e.g., oil extraction, geothermal energy production. 226Ra is a critical radionuclide in nuclear waste management, originating from e.g., nuclear industry in spent nuclear fuel or other wastes from processing uranium ore, past legacies from industry and medicine. 226Ra, is safety relevant for the deep geological disposal of spent nuclear fuel (SNF) because it is a long-lived alpha emitter (t1/2 = 1600 yrs) which dominates the radioactive dose in some scenarios regarding the late stages of SNF disposal. The prediction of 226Ra migration requires a quantitative process-understanding of the relevant retention mechanisms, i.e. adsorption, and uptake of 226Ra into a solid phase. Here we present results of experimental and theoretical studies on the structural uptake of 226Ra into the ternary solid solution of (Ba,Sr,Ra)SO4 due to the recrystallization of sulfates. This mechanism is relevant due to the fact that the solid-solutions are thermodynamically more stable than the pure phase RaSO4 and their formation leads to a lower solubility of 226Ra compared to the pure phase. The results show that already at time scales observable in the laboratory, pure sulfates are able to take up 226Ra and that their uptake can be described with thermodynamic solid-solution models. In addition, we present results regarding the adsorption of 226Ra on two important clay minerals, illite and montmorillonite. Our results show distinct differences between the selectivity of 226Ra adsorption to the two clay minerals, with a higher selectivity observed on illite. Parallel experiments with Ba indicate that 226Ra behaves similar in many geochemical conditions but is adsorbed stronger than Ba.
536 _ _ |a 1411 - Nuclear Waste Disposal (POF4-141)
|0 G:(DE-HGF)POF4-1411
|c POF4-141
|f POF IV
|x 0
700 1 _ |a Klinkenberg, Martina
|0 P:(DE-Juel1)130364
|b 1
|u fzj
700 1 _ |a Baeyens, Bart
|0 P:(DE-HGF)0
|b 2
700 1 _ |a Marquez Fernandes, Maria
|0 P:(DE-HGF)0
|b 3
700 1 _ |a Barthel, Juri
|0 P:(DE-Juel1)130525
|b 4
|u fzj
700 1 _ |a Bosbach, Dirk
|0 P:(DE-Juel1)130324
|b 5
|u fzj
909 C O |o oai:juser.fz-juelich.de:1016755
|p VDB
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 0
|6 P:(DE-Juel1)144040
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 1
|6 P:(DE-Juel1)130364
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 4
|6 P:(DE-Juel1)130525
910 1 _ |a Forschungszentrum Jülich
|0 I:(DE-588b)5008462-8
|k FZJ
|b 5
|6 P:(DE-Juel1)130324
913 1 _ |a DE-HGF
|b Forschungsbereich Energie
|l Nukleare Entsorgung, Sicherheit und Strahlenforschung (NUSAFE II)
|1 G:(DE-HGF)POF4-140
|0 G:(DE-HGF)POF4-141
|3 G:(DE-HGF)POF4
|2 G:(DE-HGF)POF4-100
|4 G:(DE-HGF)POF
|v Nukleare Entsorgung
|9 G:(DE-HGF)POF4-1411
|x 0
914 1 _ |y 2023
920 1 _ |0 I:(DE-Juel1)IEK-6-20101013
|k IEK-6
|l Nukleare Entsorgung
|x 0
920 1 _ |0 I:(DE-Juel1)ER-C-2-20170209
|k ER-C-2
|l Materialwissenschaft u. Werkstofftechnik
|x 1
980 _ _ |a talk
980 _ _ |a VDB
980 _ _ |a I:(DE-Juel1)IEK-6-20101013
980 _ _ |a I:(DE-Juel1)ER-C-2-20170209
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IFN-2-20101013


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