4.7 Article

Long-range transport of gaseous 131I and other radionuclides from Fukushima accident to Southern Poland

Journal

ATMOSPHERIC ENVIRONMENT
Volume 91, Issue -, Pages 137-145

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2014.03.065

Keywords

Atmospheric radionuclides; Fukushima accident; Radiocesium; Chernobyl; Plutonium; Radioactive fallout

Funding

  1. National Centre for Research and Development (NCBiR)
  2. Research Task Development of methods to assure nuclear safety and radiation protection for current and future needs of nuclear power plants [SP/J/6/143339/11]

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A serious accident at Fukushima Dai-Ichi NPP triggered radioactive emission to the atmosphere on 12 March 2011. The results of gamma spectrometric measurements of both gaseous and aerosol fraction of the air, collected in Krakow over the period from March 21 till the end of May 2011, as well as wet and dry deposition recorded from March till the end of October 2011, are presented in this paper. Krakow happened to be the first Polish location where radioactive isotopes characteristic for reactor releases, such as I-131, I-132, Te-129m, Te-132, (CS)-C-134, Cs-136, and Cs-137, were detected. The maximum activity for aerosols equal to (5.73 +/- 0.35) mBq/m(3), (0.461 +/- 0.041) mBq/m(3) and (0.436 +/- 0.038) mBq/m(3) for I-131, Cs-134 and Cs-137, respectively, was recorded for March 29, 2011. The data on the fallout are also given. The results of the radiochemical analysis of aerosol samples showed no traces of plutonium or americium isotopes associated with the disaster to be detected. The results of air activity concentration from Fukushima accident observed in Central Europe, Poland, in comparison to those of Chernobyl accident observed in Japan are presented and discussed. The comparison has revealed a discrepancy in the recognized relative scale of both accidents, and important difference in long distance transport of contamination, to exist. An attempt to explain the variation in the activity ratios between the aerosol fraction for I-131 and Cs-137 as resulting from exchange between the gaseous and aerosol fractions of I-131 while the contamination had been propagating, is made. (C) 2014 Elsevier Ltd. All rights reserved.

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