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U.S. Department of Energy
Office of Scientific and Technical Information

Natural repository analogue program. Progress report, October 1-December 31, 1980

Technical Report ·
DOI:https://doi.org/10.2172/6480889· OSTI ID:6480889
One fission product, molybdenum, has been found in rocks which were taken at distances between 1 and 40 meters from reactor zones. We conclude that this molybdenum was mobilized in the nearby zones of criticality, transported over distances up to a few tens of meters and redeposited in these rocks. In contrast, the same samples contain undetectable quantities of both fissiogenic ruthenium or of the /sup 235/U depleted reactor fuel. The redistribution processes enriched molybdenum by several orders of magnitude relative to ruthenium and uranium. Analyses of the source region will determine whether fractionation of these elements is due to selective mobilization at the source or preferential deposition at the repository. Ores peripheral to reactor zones are, on the average, deficient in one half of the radiogenic lead (approx. 7000 ppM). Rocks from the conglomerate underlying the mineralized stratum contain, on the average, 6000 ppM of excess lead. One sample contains a remarkable 34,000 ppM of unsupported radiogenic lead. This basal conglomerate must have been a major transport path and repository for lead lost from the ores. Additional samples from this stratum have been taken over distances up to 300 meters from the ore zones and are being analyzed to determine the extent of lead transport over these distances. The development of methods to prepare and characterize low oxygen fugacity waters has been delayed by problems in the installation of controlled atmosphere boxes.
Research Organization:
Los Alamos Scientific Lab., NM (USA)
DOE Contract Number:
W-7405-ENG-36
OSTI ID:
6480889
Report Number(s):
LA-8743-PR
Country of Publication:
United States
Language:
English