文摘
Any migration of radionuclides from nuclear wasterepositories is expected to be mitigated by adsorption tothe host rocks surrounding hydraulically conductive fractures.Fluid rock interfaces are considered to be importantbarriers for nuclear waste disposal schemes but theiradsorptive capacity can be affected by the growth ofmicrobial biofilms. This study indicates that biofilms growingon fracture surfaces decrease the rocks adsorptioncapacity for migrating radionuclides except for trivalentspecies. Potential suppression of adsorption by biofilmsshould, therefore, be accounted for in performance safetyassessment models. In this study, the adsorptive capacityof in situ anaerobic biofilms grown 450 m underground oneither glass or granite slides was compared to thecapacity of the same surfaces without biofilms. Surfaceswere exposed to the radiotracers 60Co(II), 147Pm(III),241Am(III), 234Th(IV), and 237Np(V) for a period of 660 h in apH neutral anaerobic synthetic groundwater. Adsorptionwas investigated at multiple time points over the 660 h usingliquid scintillation and ICP-MS. Results indicate thatthese surfaces adsorb between 0 and 85% of the addedtracers under the conditions of the specific experiments.After 660 h, the distribution coefficients, R (ratio betweenwhat is sorbed and what is left in the aqueous phase),approached 3 × 104 m for 60Co, 3 × 105 m for 147Pm and241Am, 1 × 106 m for 234Th, and 1 × 103 m for 237Np. The highestrate of adsorption was during the first 200 h of theadsorption experiments and started to approach equilibriumafter 500 h. Adsorption to colloids and precipitatescontributed to decreases of up to 20% in the available60Co, 147Pm, 241Am, and 237Np in the adsorption systems. Inthe 234Th system 95% of the aqueous 234Th was removedby adsorbing to colloids. Although the range of R values foreach surface tested generally overlapped, the biofilmsconsistently demonstrated lower R values except for thetrivalant 147Pm and 241Am adsorption systems.