Stratospheric fallout of bomb-produced cerium isotopes and atmospheric fractionation of nuclear debris
Levels of Ce141, Ce143 and Ce144 in individual samples of rain and snow have been measured radiochemically at Fayetteville, Arkansas, during the past few years. The data are compared with the Sr89, Sr90 and Ba140 data also obtained at Fayetteville, Arkansas. The concentrations of both radiocerium and radiostrontium show a marked seasonal variation with a peak in the spring and a minimum in the fall. During a nuclear test suspension period, the Ce141/Ce144 ratios in a series of rainfalls can be expressed as a simple function of the decay constants of Ce141 and Ce144 and the time elapsed since the cessation of the nuclear test series. The Sr89 /Sr90 ratio data, however, tend to deviate from such a theoretical equation and show a considerable scatter of experimental points. The Ce144/Sr90 ratio data, on the other hand, can not be expressed as a simple function of the decay constants and time. These results are tentatively explained as due to the effects of fractionation of the bomb-produced fission products in the atmosphere.
- Research Organization:
- Arkansas. Univ., Fayetteville, AR (United States)
- Sponsoring Organization:
- US Atomic Energy Commission (AEC)
- NSA Number:
- NSA-18-039485
- OSTI ID:
- 4020157
- Report Number(s):
- CONF-337--43
- Country of Publication:
- United States
- Language:
- English
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