Reference : Hydrogeological modeling of radionuclide transport in low permeability media: a comparis...
Scientific journals : Article
Engineering, computing & technology : Geological, petroleum & mining engineering
http://hdl.handle.net/2268/3378
Hydrogeological modeling of radionuclide transport in low permeability media: a comparison between Boom Clay and Ypresian Clay
English
Huysmans, Marijke [Katholieke Universiteit Leuven - KUL > Geologie-Geografie > Hydrogeologie en Ingenieursgeologie > >]
Dassargues, Alain mailto [Université de Liège - ULg > Département Argenco : Secteur GEO3 > Hydrogéologie & Géologie de l'environnement >]
2006
Environmental Geology
Springer Science & Business Media B.V.
50
1
122-131
Yes (verified by ORBi)
International
0943-0105
New York
NY
[en] waste disposal ; radionuclide transport ; heterogeneous media ; geostatistics ; Ypresian clay ; Boom clay
[en] Deep low-permeability clay layers are considered as suitable environments for disposal of high-level radioactive waste. In Belgium, the Boom Clay is the reference host formation and the Ypresian Clay an alternative host formation for research and safety and feasibility assessment of deep disposal of nuclear waste. In this study, two hydrogeological models are built to calculate the radionuclide fluxes that would migrate from a potential repository through these two clay formations. Transport parameter heterogeneity is incorporated in the models using geostatistical co-simulations of hydraulic conductivity, diffusion coefficient and diffusion accessible porosity. The calculated radionuclide fluxes in the two clay formations are compared. The results show that in the Ypresian Clay larger differences between the fluxes through the lower and the upper clay boundary occur, larger total output radionuclide amounts are calculated and a larger effect of parameter heterogeneity on the calculated fluxes is observed, compared to the Boom Clay.
Aquapôle - AQUAPOLE
Researchers ; Professionals
http://hdl.handle.net/2268/3378
10.1007/s00254-006-0191-7
http://www.springerlink.com/content/k3w6q86n32527137/
All our acknowledgements to Springer. The original version of this publication is available at www.springer.com

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