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Title: Use of plutonium isotope activity ratios in dating recent sediments. [/sup 238/Pu//sup 239/Pu + /sup 240/Pu]

Technical Report ·
DOI:https://doi.org/10.2172/5653421· OSTI ID:5653421

The majority of plutonium presently in the biosphere has come from the testing of nuclear devices. In the early 1950s, the Pu-238/239+240 activity ratio of fallout debris was > 0.04; in the more extensive test series of 1961 to 1962, the Pu-238/239+240 activity ratios were quite consistent at 0.02 to 0.03 and maximum fallout delivery occurred in mid-1963. A significant perturbation in Pu isotope activity ratios occurred in mid-1966 with the deposition of Pu-238 from the SNAP-9A reentry and burn-up. Recently deposited sediments have recorded these events and where accumulation rates are rapid (> 1 cm/y), changes in Pu isotope activity ratios can be used as a geochronological tool.

Research Organization:
Oregon State Univ., Newport (USA). Marine Science Center
Sponsoring Organization:
USDOE
DOE Contract Number:
AT06-76EV70030
OSTI ID:
5653421
Report Number(s):
DOE/EV/70030-9; ON: DE82011082; TRN: 82-008994
Country of Publication:
United States
Language:
English