In this work, we have studied the sorption of selenium (79Se is one of the main radionuclides in a spent nuclear fuel repository) on magnetite (Fe3O4), a mineral present in the near-field of a nuclear waste repository that might represent an important retardation factor for the mobility of many radionuclides.
The sorption of both Se(IV) and Se(VI) onto magnetite has been fitted by a non-competitive Langmuir isotherm with Γmax = (3.13 ± 0.07) × 10−6 mol m−2 and KL = (1.19 ± 0.07) × 106 dm3 mol−1 for Se(IV) and Γmax = (3.5 ± 0.2) × 10−6 mol m−2 and KL = (3.0 ± 0.1) × 105 dm3 mol−1 for Se(VI).
The variation of the sorption of selenium with pH has been modeled using the Triple Layer Surface Complexation Model and the equilibrium constants between selenium and magnetite have been obtained using the FITEQL program. For the case of Se(IV), the best fitting has been obtained using two inner-sphere complexes, >FeOHSeO32− and >FeHSeO3, while for Se(VI), the best fitting has been obtained considering only an outer-sphere complex, >FeOH2+—SeO42−. |
