The influence of sedimentary heterogeneity on the diffusion of radionuclides in the sandy facies of Opalinus Clay at the field scale
Chaofan Chen
Helmholtz Centre for Environmental Research-UFZ, Permoser Str. 15, 04318 Leipzig, Germany
School of Energy and Mining Engineering, China University of Mining and Technology (Beijing), 100083 Beijing, China
Department of Reactive Transport, Institute of Resource Ecology, Helmholtz-Zentrum Dresden-Rossendorf (HZDR), 04318 Leipzig, Germany
Department of Geosciences, University of Tübingen, 72076 Tübingen, Germany
Renchao Lu
Helmholtz Centre for Environmental Research-UFZ, Permoser Str. 15, 04318 Leipzig, Germany
Cornelius Fischer
Department of Reactive Transport, Institute of Resource Ecology, Helmholtz-Zentrum Dresden-Rossendorf (HZDR), 04318 Leipzig, Germany
Olaf Kolditz
Helmholtz Centre for Environmental Research-UFZ, Permoser Str. 15, 04318 Leipzig, Germany
Applied Environmental Systems Analysis, Dresden University of Technology, 01069 Dresden, Germany
Haibing Shao
Helmholtz Centre for Environmental Research-UFZ, Permoser Str. 15, 04318 Leipzig, Germany
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Short summary
The moving distance of the diffusion front is farther away the canister center, along the direction with the neighboring layer having lower diffusion coefficient.
When the bedding angle increases, the diffusion front moves farther in z+ direction, reflecting the increase in effective diffusivity and higher impact of parallel-to-bedding diffusion.
The neighboring layers can slightly reshape the diffusion front line of the radionuclide.
The moving distance of the diffusion front is farther away the canister center, along the...