“…It seems, therefore, that both iodide and selenite are effectively non-sorbing in the rock core investigated in this work. For iodide, this is expected (André et al, 2009;Ohlsson and Neretnieks, 1997), while for selenite the results from batch experiments with crushed rocks suggested that it is a weakly sorbing species, with 𝐾 d values on the order of 2.95×10 -4 m 3 /kg for Forsmark and Laxemar granites (Crawford, 2010) and 2.0×10 -3 m 3 /kg for Grimsel granodiorite (Li et al, 2018). We found, however, that the assumption of selenite as a sorbing species always made the curvature of the simulated breakthrough curves to deviate clearly from that obtained in the experiments, especially at the moments around the breakthrough time, when the advection-dispersion model or the reactive transport model was used.…”