Long-term diffusion of U(VI) in bentonite: Dependence on density
Creators
- 1. Glenn T. Seaborg Institute, Physical & Life Sciences Directorate, Lawrence Livermore National Laboratory, L-231, P.O. Box 808, Livermore, CA 94550 (United States)
- 2. Helmholtz-Zentrum Dresden-Rossendorf e.V., Institute of Resource Ecology, P.O. Box 510119, 01314 Dresden (Germany)
- 3. Biosciences and Biotechnology Division, Physical & Life Sciences Directorate, Lawrence Livermore National Laboratory, L-231, P.O. Box 808, Livermore, CA 94550 (United States)
Description
As a contribution to the safety assessment of nuclear waste repositories, U(VI) diffusion through the potential buffer material MX-80 bentonite was investigated at three clay dry densities over six years. Synthetic MX-80 model pore water was used as background electrolyte. Speciation calculations showed that Ca2UO2(CO3)3(aq) was the main U(VI) species. The in- and out-diffusion of U(VI) was investigated separately. U(VI) diffused about 3 mm, 1.5 mm, and 1 mm into the clay plug at ρ = 1.3, 1.6, and 1.9 g/cm3, respectively. No through-diffusion of the U(VI) tracer was observed. However, leaching of natural uranium contained in the clay occurred and uranium was detected in all receiving reservoirs. As expected, the effective and apparent diffusion coefficients, De and Da, decreased with increasing dry density. The Da values for the out-diffusion of natural U(VI) were in good agreement with previously determined values. Surprisingly, Da values for the in-diffusion of U(VI) were about two orders of magnitude lower than values obtained in short-term in-diffusion experiments reported in the literature. Some potential reasons for this behavior that were evaluated are changes of the U(VI) speciation within the clay (precipitation, reduction) or changes of the clay porosity and pore connectivity with time. By applying Archie's law and the extended Archie's law, it was estimated that a significantly smaller effective porosity must be present for the long-term in-diffusion of U(VI). The results suggest that long-term studies of key transport phenomena may reveal additional processes that can directly impact long-term repository safety assessments. - Highlights: • Nuclear waste repository risk assessment requires long-term U-diffusion data. • U(VI) diffusion in bentonite was investigated over 6 years. • U-diffusion was about 100 times lower than published in short-term studies. • Clay porosity and pore connectivity may change with time and hinder diffusion. • Lower U-diffusivities substantially improve long-term repository safety.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2016.10.005Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2016.10.005;
- PII
- S0048-9697(16)32170-2;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 575
- Journal Page Range
- p. 207-218
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 49065660
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- BENTONITE; DENSITY; DIFFUSION; NATURAL URANIUM; POROSITY; RADIOACTIVE WASTES; RISK ASSESSMENT; SAFETY; SOCIO-ECONOMIC FACTORS
- Descriptors DEC
- ACTINIDES; CLAYS; ELEMENTS; INORGANIC ION EXCHANGERS; INSTITUTIONAL FACTORS; ION EXCHANGE MATERIALS; MATERIALS; METALS; MINERALS; PHYSICAL PROPERTIES; RADIOACTIVE MATERIALS; SILICATE MINERALS; URANIUM; WASTES
Optional Information
- Copyright
- Copyright (c) 2016 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.