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Title: {sup 55}Fe concentration and specific activities in north Pacific marine organisms

Technical Report ·
DOI:https://doi.org/10.2172/10188073· OSTI ID:10188073

The {sup 55}Fe from nuclear weapons testing which enters the ocean is in a chemical form which is much more readily available for biological uptake than is stable oceanic iron. This property of {sup 55}Fe results in up to 1000-fold higher {sup 55}Fe specific activities in marine organisms than is present in seawater. Dilution of {sup 55}Fe by stable iron from anthropogenic sources or natural sources appears to be responsible for the lower specific activity in mid-latitude marine organisms than in organisms from high latitudes. The half-time for {sup 55}Fe in harvested salmon from the west coast is essentially the same as the half-residence time for stratospheric radioactive debris. This fact suggests that {sup 55}Fe reaching the ocean surface is available for biological uptake for a relatively short time. Measurements of {sup 55}Fe specific activities in certain crustacea predacious fish than in the phytoplankton. What we have learned about the behavior of the radionuclide {sup 55}Fe in the ocean environment may well apply to other fallout radionuclides, and a consideration of this fact should be included in estimating the potential hazard of the release of radionuclides to the marine environment. These data suggest that the release of radioiron from a reactor to the oceans at northern latitudes may have a 10 to 30-fold greater impact than releases of radioiron at mid-latitudes.

Research Organization:
Battelle Pacific Northwest Lab., Richland, WA (United States)
Sponsoring Organization:
USDOE, Washington, DC (United States)
DOE Contract Number:
AC06-76RL01830
OSTI ID:
10188073
Report Number(s):
BNWL-SA-4662; ON: DE93001727
Resource Relation:
Other Information: PBD: [1972]
Country of Publication:
United States
Language:
English