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A Method for Continuous (239)Pu Determinations in Arctic and Antarctic Ice Cores
M M Arienzo1, J R McConnell1, N Chellman1
1Desert Research Institute , 2215 Raggio Parkway, Reno, Nevada 89512, United States.
A new method for measuring plutonium-239 (Pu) in ice cores allows for continuous, semiquantitative analysis of nuclear weapons testing (NWT) fallout. This technique provides annual records from Greenland and Antarctica, improving upon previous methods.
Area of Science:
- Environmental Science
- Radiochemistry
- Paleoclimatology
Background:
- Atmospheric nuclear weapons testing (NWT) led to global plutonium (Pu) deposition.
- Previous methods for Pu analysis in ice cores were time-consuming and had lower resolution.
- Understanding past NWT fallout is crucial for environmental monitoring.
Purpose of the Study:
- To develop and validate a new method for continuous semiquantitative measurement of plutonium-239 (Pu) in ice cores.
- To establish annual records of NWT fallout in Greenland and Antarctic ice cores.
- To demonstrate the advantages of the new continuous measurement technique.
Main Methods:
- Direct measurement of plutonium-239 (Pu) using inductively coupled plasma-sector field mass spectrometry.
- Continuous analysis of ice cores from Greenland and Antarctica.
- Validation by comparing results with published Pu records and NWT data.
Main Results:
- Annual records of plutonium-239 (Pu) fallout from NWT were successfully developed for ten ice cores.
- Arctic Pu profiles reflected global NWT trends and agreed with lower latitude ice core data.
- Antarctic Pu measurements correlated with low latitude NWT, consistent with prior Antarctic studies.
Conclusions:
- The new continuous Pu measurement method significantly reduces analysis time and sample requirements.
- This method allows for precise coregistration of Pu data with other ice core analyses.
- The stable Pu-239 record provides a valuable, long-term archive of NWT fallout.
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