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@ARTICLE{Poonoosamy:1007367,
author = {Poonoosamy, Jenna and Kaspor, Alexander and Rudin, Stefan
and Murphy, Gabriel L. and Bosbach, Dirk and Deissmann,
Guido},
title = {{T}he {U}se of {M}icrofluidic {P}latforms with {R}aman
{S}pectroscopy for {I}nvestigating the {C}o-{P}recipitation
of {M}etals and {R}adionuclides in {C}arbonates},
journal = {Minerals},
volume = {13},
number = {5},
issn = {2075-163X},
address = {Basel},
publisher = {MDPI},
reportid = {FZJ-2023-02032},
pages = {636 -},
year = {2023},
abstract = {In the context of long-term safety assessments of deep
geological repositories for radio-active wastes, a rigorous
understanding of the retention of radionuclides such as
226Ra due to co-precipitation with carbonate and sulphate
minerals is important for a realistic prediction of
radionuclide migration behaviour in the repository near and
far field. The co-precipitation of 226Ra in sulphate
minerals, in particular barite, has been studied
experimentally and numerically in detail throughout the last
decade to establish the thermodynamic properties and mixing
behaviour of its solid solutions over a wide range of
temperatures. However, so far, few studies have been
dedicated to the incorporation of 226Ra into carbonates, and
little is known about the mixing behaviour of 226Ra and
calcium carbonate phases such as calcite, aragonite, or
vaterite. The aim of the work presented here was to develop
and explore innovative microfluidic experiments in
combination with in situ Raman spectroscopy that can be used
to investigate co-precipitation processes of radionuclides
in carbonate minerals, using stable Ba as a chemical
analogue for 226Ra in the first step, due to their similar
ionic radii. Different microfluidic set-ups were developed
to address co-precipitation in bulk solution as well as in
confinement or under diffusive flow regimes. It could be
shown by XRD and SEM-EDX analyses that high amounts of Ba
can be incorporated into the lattice of calcite when formed
via an amorphous precursor phase, suggesting that the
formation of calcium carbonates can contribute to the
retention of 226Ra in the repository environment, which will
be verified in future studies using the presented
microfluidic platforms.},
cin = {IEK-6},
ddc = {550},
cid = {I:(DE-Juel1)IEK-6-20101013},
pnm = {1411 - Nuclear Waste Disposal (POF4-141) / Verbundprojekt:
Verhalten langlebiger Spalt- und Aktivierungsprodukte im
Nahfeld von Endlagern unterschiedlicher Wirtsgesteine und
Möglichkeiten ihrer Rückhaltung (VESPA II), Teilprojekt D
(02E11607D)},
pid = {G:(DE-HGF)POF4-1411 / G:(BMWi)02E11607D},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000997228800001},
doi = {10.3390/min13050636},
url = {https://juser.fz-juelich.de/record/1007367},
}