Isotopic evidence of plutonium release into the environment from the Fukushima DNPP accident.
(Source)
http://www.ncbi.nlm.nih.gov/pubmed/22403743
Abstract
The
Fukushima Daiichi nuclear power plant (DNPP) accident caused massive
releases of radioactivity into the environment. The released highly
volatile fission products, such as (129m)Te, (131)I, (134)Cs, (136)Cs
and (137)Cs were found to be widely distributed in Fukushima and its
adjacent prefectures in eastern Japan. However, the release of
non-volatile actinides, in particular, Pu isotopes remains uncertain
almost one year after the accident. Here we report the isotopic
evidence for the release of Pu into the atmosphere and deposition on
the ground in northwest and south of the Fukushima DNPP in the
20-30 km zones. The high activity ratio of (241)Pu/(239+240)Pu (>
100) from the Fukushima DNPP accident highlights the need for
long-term (241)Pu dose assessment, and the ingrowth of (241)Am. The
results are important for the estimation of reactor damage and have
significant implication in the strategy of decontamination.
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