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@INPROCEEDINGS{Brandt:140944,
author = {Brandt, Felix and Klinkenberg, Martina and Breuer, Uwe and
Rozov, Konstantin and Bosbach, Dirk},
title = {{U}ptake of {R}adium during barite recrystallization},
reportid = {FZJ-2013-06165},
year = {2013},
abstract = {In recent safety assessments for the direct disposal of
spent nuclear fuel, Ra has been identified as a main
contributor to dose after 100,000 years [1]. Due to the
likely presence of BaSO4 which is formed by a reaction of Ba
present as a fission product and sulfate ubiquitous in
ground waters, it is expected that Ra will form a
RaxBa1-xSO4 solid solution via recrystallization, which
would lower the Ra concentration in solution significantly.
However, due to a lack of reliable data, this solid solution
system is currently not considered in long term safety
assessments for nuclear waste repositories. For instance,
the solubility of the pure RaSO4 endmember is not well
defined. Furthermore, available literature data for the
interaction parameter a0, which describes the non-ideality
of the solid solution, vary by about one order of magnitude
[2, 3]. The final Ra concentration in solution in this
system is extremely sensitive to the amount of barite
present, the difference in the solubility products of the
end-member phases, and the degree of non-ideality of the
solid solution phase. The EU-funded SKIN project
investigates slow processes in close-to-equilibrium
conditions for radionuclides in water/solid systems of
relevance to nuclear waste management. Within the SKIN
project we have combined a macroscopic experimental approach
with ToF-SIMS and thermodynamic modelling to study in detail
how a Ra containing solution will equilibrate with solid
BaSO4 under repository relevant conditions. Batch
experiments at close to equilibrium conditions show a final
Ra concentration which is several orders of magnitude lower
than the solubility of pure RaSO4. For the first time, the
spatial distribution of Ra and Ba within the recrystallized
barite powders - analysed using an ION-TOF TOF-SIMS -
confirms the uptake of Ra into the solid. Solid-solution
aqueous-solution equilibrium calculations were carried out
for the BaSO4 – RaSO4 – H2O system with the GEMS – PSI
code [4] in combination with the NAGRA – PSI thermodynamic
database [10]. Thermodynamic modelling fits the experimental
data best with an interaction parameter a0 = 0.6 and a
solubility product KRaSO4 = -10.41.[1] Norrby, S.;
Andersson, J.; Dverstorp, B.; Kautsky, F.; Lilja, C.;
Sjöblom, R.; Sundström, B.; Toverud, Ö. $\&$ Wingefors,
S. SKB 1997[2] Zhu, C. Geochimica et Cosmochimica Acta,
2004, 68, 3327-3337[3] Curti, E.; Fujiwara, K.; Iijima, K.;
Tits, J.; Cuesta, C.; Kitamura, A.; Glaus, M. $\&$ Müller,
W. Geochimica et Cosmochimica Acta, 2010, 74, 3553-3570[4]
Wagner, T.; Kulik, D.; Hingerl, F. $\&$ Dmytrieva, S.
Canadian Mineralogist, 2012, 50, 701 - 723[5] Hummel, W.;
Berner, U.; Curti, E.; Pearson, F. J. $\&$ Thoenen, T.;
Nagra technical report 02-16 2002},
month = {Oct},
date = {2013-10-14},
organization = {EURADWASTE ’13, 8th EC Conference on
the Management of Radioactive Waste
Community Policy and Research on
Disposal, Vilnius (Lithuania), 14 Oct
2013 - 17 Oct 2013},
cin = {IEK-6 / ZEA-3},
cid = {I:(DE-Juel1)IEK-6-20101013 / I:(DE-Juel1)ZEA-3-20090406},
pnm = {142 - Safety Research for Nuclear Waste Disposal (POF2-142)
/ SKIN - Slow processes in close-to-equilibrium conditions
for radionuclides in water/solid systems of relevance to
nuclear waste management (269688)},
pid = {G:(DE-HGF)POF2-142 / G:(EU-Grant)269688},
typ = {PUB:(DE-HGF)24},
url = {https://juser.fz-juelich.de/record/140944},
}