Environmental Management Science Program Research in Michigan
59849 - Radionuclide Immobilization in the Phases Formed by Corrosion
of Spent Nuclear Fuel: The Long-Term Assessment
Year of Award: |
1997 |
Amount of Award: |
$480,963 |
Problem Area: |
Spent Nuclear Fuel |
Science Categories/SubCategories: |
Geochemistry / Solid/Solution Geochemistry (primary)
Materials Science / Surface Chemistry
Inorganic Chemistry / Solid/Solution Chemistry |
Lead Principal Investigator: |
Dr. Rodney C. Ewing
3003 S. State Street
University of Michigan
Ann Arbor, Michigan 48109
313-647-8529, rodewing@umich.edu |
For More Information: |
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Description Provided by Investigator:
The UO2 in spent nuclear fuel is not stable under oxidizing conditions.
Under oxic conditions, the U(IV) has a strong tendency to exist as U(VI) in the uranyl
molecule, UO22+. The uranyl ions react with a wide variety of
inorganic and organic anions to form complexes which are often highly soluble. The result
is rather rapid dissolution of UO2 and the formation of a wide variety of
uranyl oxide hydrates, uranyl silicates and uranyl phosphates. The reaction rates for this
transformation are rapid, essentially instantaneous on geologic time scales. Over the long
term, and depending on the extent to which these phases can incorporate fission products
and actinides, these alteration phases become the near-field source term.
Fortunately, previous investigations (experimental studies and field studies) have
established that natural uraninites and their alteration products can be used as natural
analogues to study the corrosion of UO2 in spent nuclear fuel. We propose
in this research program to address the following issues:
- What are the long-term corrosion products of natural UO2+x, uraninite, under
oxidizing conditions?
- What is the paragenesis or the reaction path of the phases that form during alteration?
How is the paragenetic sequence formation related to the structures and compositions of
these uranyl phases?
- What is the trace element content (as compared to the original UO2+x), and
does the trace element content substantiate models developed to predict fission product
and actinide incorporation into these phases?
- Are these the phases that are predicted from reaction path models (e.g., EQ3/6) which
will be used in performance assessments?
- How persistent over time are the metastable phase assemblages that form? Will these
phases serve as barriers to radionuclide release?
- Based on the structures of these phases (mostly sheet structures) can the thermodynamic
stabilities of these phases be estimated, or at least bounded, in such a way as to provide
for a convincing and substantive performance assessment?
This research is based on over a decade of previous work on uranium mineralogy,
paragenesis, and the corrosion of UO2 by the principal investigator, R. C.
Ewing.
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