Predictive and inverse modeling of a radionuclide diffusion experiment in crystalline rock at ONKALO (Finland)

オンカロ地下特性調査施設における結晶質岩中の放射性核種拡散試験の予測解析と逆解析

Soler, J. M.*; Keklinen, P.*; Pulkkanen, V.-M.*; Moreno, L.*; Iraola, A.*; Trinchero, P.*; Hokr, M.*; ha, J.*; Havlov, V.*; Trpkoov, D.*; Vetenk, A.*; Voplka, D.*; Gvodk, L.*; Milick, M.*; Polk, M.*; 深津 勇太  ; 伊藤 剛志*; 舘 幸男  ; Svensson, U.*; Park, D. K.*; Ji, S.-H.*; Gylling, B.*; Lanyon, G. W.*

Soler, J. M.*; Keklinen, P.*; Pulkkanen, V.-M.*; Moreno, L.*; Iraola, A.*; Trinchero, P.*; Hokr, M.*; ha, J.*; Havlov, V.*; Trpkoov, D.*; Vetenk, A.*; Voplka, D.*; Gvodk, L.*; Milick, M.*; Polk, M.*; Fukatsu, Yuta; Ito, Tsuyoshi*; Tachi, Yukio; Svensson, U.*; Park, D. K.*; Ji, S.-H.*; Gylling, B.*; Lanyon, G. W.*

The REPRO-TDE test was performed at a depth of about 400 m in the ONKALO underground research facility in Finland. Synthetic groundwater containing radionuclide tracers (HTO, Cl-36, Na-22, Ba-133, Cs-134) was circulated for about four years in a packed-off interval of the injection borehole. Tracer activities were additionally monitored in two observation boreholes. The test was the subject of a modelling exercise by the SKB GWFTS Task Force. Eleven teams participated in the exercise, using different model concepts and approaches. Predictive model calculations were based on laboratory-based information concerning porosities, diffusion coefficients and sorption partition coefficients. After the experimental results were made available, the teams were able to revise their models to reproduce the observations. General conclusions from these back-analysis calculations include the need for reduced effective diffusion coefficients for Cl-36 compared to those applicable to HTO (anion exclusion), the need to implement weaker sorption for Na-22, compared to results from laboratory batch-sorption experiments, and the observation of large differences between the theoretical initial concentrations for the strongly-sorbing Ba-133 and Cs-134 and the first measured values a few hours after tracer injection. Different teams applied different concepts, concerning mainly the implementation of isotropic vs. anisotropic diffusion, or the possible existence of Borehole Disturbed Zones around the different boreholes. The role of microstructure was also addressed in two of the models.