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Carbon-14 in waste packages for spent fuel in a tuff repository

Technical Report ·
DOI:https://doi.org/10.2172/59998· OSTI ID:59998

Carbon-14 is produced naturally by cosmic ray neutrons in the upper atmosphere. It is also produced in nuclear reactors, in amounts much smaller than the global inventory. About one-third of this is released directly to the atmosphere, and the other two-thirds remains in the spent fuel. Both the Environmental Protection Agency and the Nuclear Regulatory Commission have established limits on release of the {sup 14}C in spent fuel. This is of particular concern for the proposed repository in tuff, because of the unsaturated conditions and the consequent possibility of gaseous transport of {sup 14}C as CO{sub 2}. Existing measurements and calculations of the {sup 14}C inventory in spent fuel are reviewed. The physical distribution and chemical forms of the {sup 14}C are discussed. Available data on the release of {sup 14}C from spent fuel in aqueous solutions and in gaseous environments of air, nitrogen, and helium are reviewed. Projected {sup 14}C behavior in a tuff repository is described. It is concluded that {sup 14}C release measurements from spent fuel into moist air at temperatures both above and below the in situ boiling point of water as well as detailed transport calculations for the tuff geological environment will be needed to determine whether the 10CFR60 and 40CFR191 requirements can be met. 56 refs., 1 tab.

Research Organization:
Lawrence Livermore National Lab., CA (United States); Hanford Engineering Development Lab., Richland, WA (United States)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
59998
Report Number(s):
UCRL--94708; CONF-861207--31; ON: DE87004365
Country of Publication:
United States
Language:
English

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