Comparison of Pu and (137)Cs as tracers of soil and sediment transport in a terrestrial environment.
Following atmospheric nuclear weapons testing in the 1950s and 1960s significant quantities of (137)Cs and (239+240)Pu were deposited worldwide. In recent decades, (137)Cs has been commonly used as a tracer of soil erosion and sedimentation, particularly in the Northern Hemisphere where atomic deposition was three times as great as in the Southern Hemisphere. The relatively short 30-year half-life of this isotope means that its sensitivity as a tracer is rapidly decreasing. In contrast, with half-lives of 24,110 and 6561 years, the sensitivity of the two plutonium isotopes remains essentially the same as when it was deposited. Here we use the technique of Accelerator Mass Spectrometry to demonstrate the potential of anthropogenic Pu as an alternative to (137)Cs as a tracer of soil transport in Australia. We measure an average (137)Cs/(239+240)Pu activity ratio of 27.3+/-1.5 and an average (240)Pu/(239)Pu atom ratio of 0.149+/-0.003, both slightly lower than the global average.
Department of Nuclear Physics, Research School of Physical Sciences and Engineering, The Australian National University, Building 57, Canberra, 0200 ACT, Australia. sarah.everett@anu.edu.au
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Everett
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Bartley
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Fifield
D002588:Cesium Radioisotopes / Q000032:analysis*; D019015:Geologic Sediments / Q000737:chemistry*; D006207:Half-Life; D011005:Plutonium / Q000032:analysis*; D012990:Soil Pollutants, Radioactive / Q000032:analysis*; D014875:Water Pollutants, Radioactive / Q000032:analysis*
D002588:Cesium Radioisotopes; D012990:Soil Pollutants, Radioactive; D014875:Water Pollutants, Radioactive; D011005:Plutonium