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Modelling of the LTDE-SD radionuclide diffusion experiment in crystalline rock at the Äspö Hard Rock Laboratory (Sweden)

Authors :
Ministerio de Ciencia e Innovación (España)
Soler, Josep M.
Meng, Shuo
Moreno Zamora, Luis Ricardo
Neretnieks, Ivars
Liu, Longcheng
Kekäläinen, Pekka
Hokr, Milan
Říha, Jakub
Vetešník, Aleš
Reimitz, Dan
Višňák, Jakub
Vopálka, Dušan
Kröhn, Klaus Peter
Tachi, Yukio
Ito, Tsuyoshi
Svensson, Urban
Iraola, Aitor
Trinchero, Paolo
Voutilainen, Mikko
Deissmann, Guido
Bosbach, Dirk
Park, Dong Kyu
Ji, Sung Hoon
Gvoždík, Libor
Milický, Martin
Polák, Michal
Gylling, Björn
William Lanyon, G.
Ministerio de Ciencia e Innovación (España)
Soler, Josep M.
Meng, Shuo
Moreno Zamora, Luis Ricardo
Neretnieks, Ivars
Liu, Longcheng
Kekäläinen, Pekka
Hokr, Milan
Říha, Jakub
Vetešník, Aleš
Reimitz, Dan
Višňák, Jakub
Vopálka, Dušan
Kröhn, Klaus Peter
Tachi, Yukio
Ito, Tsuyoshi
Svensson, Urban
Iraola, Aitor
Trinchero, Paolo
Voutilainen, Mikko
Deissmann, Guido
Bosbach, Dirk
Park, Dong Kyu
Ji, Sung Hoon
Gvoždík, Libor
Milický, Martin
Polák, Michal
Gylling, Björn
William Lanyon, G.
Publication Year :
2022

Abstract

This study shows a comparison and analysis of results from a modelling exercise concerning a field experiment involving the transport and retention of different radionuclide tracers in crystalline rock. This exercise was performed within the Swedish Nuclear Fuel and Waste Management Company (SKB) Task Force on Modelling of Groundwater Flow and Transport of Solutes (Task Force GWFTS). Task 9B of the Task Force GWFTS was the second subtask within Task 9 and focused on the modelling of experimental results from the Long Term Sorption Diffusion Experiment in situ tracer test. The test had been performed at a depth of about 410m in the Äspö Hard Rock Laboratory. Synthetic groundwater containing a cocktail of radionuclide tracers was circulated for 198 days on the natural surface of a fracture and in a narrow slim hole drilled in unaltered rock matrix. Overcoring of the rock after the end of the test allowed for the measurement of tracer distribution profiles in the rock from the fracture surface (A cores) and also from the slim hole (D cores). The measured tracer activities in the rock samples showed long profiles (several cm) for non-or weakly-sorbing tracers (Cl-36, Na-22), but also for many of the more strongly-sorbing radionuclides. The understanding of this unexpected feature was one of the main motivations for this modelling exercise. However, re-evaluation and revision of the data during the course of Task 9B provided evidence that the anomalous long tails at low activities for strongly sorbing tracers were artefacts due to cross-contamination during rock sample preparation. A few data points remained for Cs-137, Ba-133, Ni-63 and Cd-109, but most measurements at long distances from the tracer source (>10mm) were now below the reported detection limits. Ten different modelling teams provided results for this exercise, using different concepts and codes. The tracers that were finally considered were Na-22, Cl-36, Co-57, Ni-63, Ba-133, Cs-137, Cd-109, Ra-226 and Np

Details

Database :
OAIster
Notes :
English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1348918123
Document Type :
Electronic Resource