Melgunov MS, Pokhilenko NP, Strakhovenko VD, Sukhorukov FV, Chuguevskii AV. Fallout traces of the Fukushima NPP accident in southern West Siberia (Novosibirsk, Russia).
Environ Sci Pollut Res Int 2012;
19:1323-1325. [PMID:
22113319 DOI:
10.1007/s11356-011-0659-1]
[Citation(s) in RCA: 6] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/01/2011] [Accepted: 11/02/2011] [Indexed: 05/31/2023]
Abstract
BACKGROUND
The fallout of artificially produced radioactive isotopes has been recorded at a site in southern West Siberia (54°50'43.6″ N, 083°06'22.4″ E, Novosibirsk, Russia).
DISCUSSION
The highest activities of (131)I, (134)Cs, and (136)Cs were found in fresh snow precipitated on 02 April 2011, at 0.83, 0.092, and 0.002 Bq L(-1) of meltwater, respectively. The (131)I/(134)Cs ratio decreased from 9.0 on 02 April to 1.2 on 27 April, which is consistent with the radioactive decay of (131)I. This fallout can only have originated from the accidental emission of Fukushima Nuclear Power Plant, Japan, in March 2011.
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