Abstract
Diffusion is the dominant process involved in the transport of 129I through geological media; therefore, the evaluation of the experimental results on the diffusion of I− through compacted bentonite was performed by three diffusion models, CC-CC, CC-VC, and VC-VC. Multiple experiments were cross-checked to verify internal consistency and thereby obtain reliable diffusion parameters. The results showed that I− diffusion coefficients ranged from 1.15 × 10–12 to 4.67 × 10–12 m2/s, which were consistent with those of the literature. These techniques could potentially be performed to measure the diffusion coefficients of non-sorbing or weakly sorbing radionuclides onto compacted bentonite in radioactive waste repositories.
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Abbreviations
- αc :
-
Capacity factor of porous medium, dimensionless
- ρb :
-
Bulk dry density of the porous medium, gcm−3
- θtot :
-
Total porosity of the porous medium; dimensionless
- Kd :
-
Distribution coefficient, cm3 g−1
- A:
-
Cross sectional area of specimen normal to the direction of the diffusional flux, cm2
- L:
-
Thickness (or length) of the specimen in the direction of diffusion, cm
- C:
-
Concentration of the diffusing substance in pore water, ppm
- CA :
-
Concentration of the diffusing substance in the inlet reservoir, ppm
- CB :
-
Concentration of the diffusing substance in the outlet reservoir, ppm
- Qt :
-
Total accumulated amount of diffusing substance, mol
- Da :
-
Apparent diffusion coefficient, m2 s-1
- De :
-
Effective diffusion coefficient, m2 s-1
- VA :
-
Volume of inlet reservoir, mL
- VB :
-
Volume of outlet reservoir, mL
- V1 :
-
Volume of specimen, mL
- S:
-
Fitted slope
- t:
-
Time, s
- tx :
-
Time-lag, s
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Tsai, TL., Tsai, SC., Chang, DM. et al. Intercomparison of determining diffusion coefficients of I− in compacted bentonite using various mathematical models of through-diffusion experiments in the laboratory. J Radioanal Nucl Chem 330, 1317–1327 (2021). https://doi.org/10.1007/s10967-021-08041-y
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DOI: https://doi.org/10.1007/s10967-021-08041-y