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U.S. Department of Energy
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Historical /sup 14/C measurements from the Atlantic, Pacific and Indian Oceans. Final report

Technical Report ·
OSTI ID:5084939

Atmospheric nuclear testing produced a dramatic increase in the level of /sup 14/C in atmospheric CO/sub 2/. Since the tropospheric residence time of /sup 14/C is on the order of a few years before being transferred to the sea, it appeared that a study of the distribution of the excess /sup 14/C in the sea and its change with time would give valuable insight into such problems as the rate of CO/sub 2/ exchange between the atmosphere and the sea and its dependence on wind speed over the sea surface; the rate of transfer by oceanic mixing processes of contaminants, including fallout radionuclides introduced initially into the mixed surface layer of the sea, into the deep sea; the rate of bottom water formation at high latitudes and subsequent advective transport from these source regions into the deep sea. Therefore a /sup 14/C sampling program was initiated. A method was developed for stripping CO/sub 2/ from sea water on board ship. The assay for /sup 14/C was performed by a radiocarbon gas proportional counter. Information on temperature and salinity at the various sampling depths as well as total CO/sub 2/ and absolute concentration of /sup 14/C is tabulated. (JGB)

Research Organization:
Washington Univ., Seattle (USA); Pacific Marine Environmental Lab., Seattle, WA (USA)
DOE Contract Number:
AT06-79EV10010
OSTI ID:
5084939
Report Number(s):
DOE/EV/10010-2; ON: DE82020639
Country of Publication:
United States
Language:
English