Articles | Volume 67
https://doi.org/10.5194/adgeo-67-35-2025
https://doi.org/10.5194/adgeo-67-35-2025
30 Oct 2025
 | 30 Oct 2025

Effect of spatial variability on uranium diffusion in the three facies of the Opalinus Clay at Mont Terri

Marco De Lucia, Marco Fabbri, and Theresa Hennig

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Cited articles

Bossart, P., Bernier, F., Birkholzer, J., Bruggeman, C., Connolly, P., Dewonck, S., Fukaya, M., Herfort, M., Jensen, M., Matray, J.-M., Mayor, J. C., Moeri, A., Oyama, T., Schuster, K., Shigeta, N., Vietor, T., and Wieczorek, K.: Mont Terri rock laboratory, 20 years of research: introduction, site characteristics and overview of experiments, Swiss Journal of Geosciences, 110, 3–22, https://doi.org/10.1007/s00015-016-0236-1, 2017. a, b, c, d
Charlton, S. R. and Parkhurst, D. L.: Modules based on the geochemical model PHREEQC for use in scripting and programming languages, Computers & Geosciences, 37, 1653–1663, https://doi.org/10.1016/j.cageo.2011.02.005, 2011. a
Chilès, J.-P. and Delfiner, P.: Geostatistics: Modeling Spatial Uncertainty, Wiley, ISBN 9781118136188, https://doi.org/10.1002/9781118136188, 2012. a
De Lucia, M., Lagneau, V., de Fouquet, C., and Bruno, R.: The influence of spatial variability on 2D reactive transport simulations, Comptes Rendus. Géoscience, 343, 406–416, https://doi.org/10.1016/j.crte.2011.04.003, 2011. a, b
De Lucia, M., Kühn, M., Lindemann, A., Lübke, M., and Schnor, B.: POET (v0.1): speedup of many-core parallel reactive transport simulations with fast DHT lookups, Geosci. Model Dev., 14, 7391–7409, https://doi.org/10.5194/gmd-14-7391-2021, 2021. a, b
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Short summary
The effect of spatial variability on uranium diffusion in Opalinus Clay over a million years was assessed by 2D reactive transport simulations. Different rock types and porosity impacted results, with variability's influence growing with longer correlation lengths of geostatistical simulations (up to 12.9 %). This highlights that 1D models may underestimate uncertainty in long-term radionuclide transport at repository sites, and spatial variability must be considered.
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