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Size distributions of airborne radionuclides from the fukushima nuclear accident at several places in europe

Authors :
Olivier Meisenberg
Magdalena Długosz-Lisiecka
W. Ringer
Petr Rulík
Konstantinos Eleftheriadis
Olivier Masson
Helena Malá
Anne de Vismes-Ott
François Gensdarmes
Laboratoire d'étude radioécologique du milieu continental et marin (LERCM)
Institut de Radioprotection et de Sûreté Nucléaire (IRSN)-Direction de l'Environnement et de l'Intervention
Austrian Agency for Health and Food Safety (AGES)
National Radiation Protection Institute (NRPI/SURO)
Institute of Applied Radiation Chemistry
Łódź University of Technology
Environmental Radioactivity laboratory (ERL)
Institute of Nuclear and Radiological Sciences and Technology, Energy and Safety (INRASTES)
National Center for Scientific Research 'Demokritos' (NCSR)-National Center for Scientific Research 'Demokritos' (NCSR)
PRP-ENV/STEME/LMRE, Laboratoire de Mesure de la Radioactivité dans l’Environnement
Institut de Radioprotection et de Sûreté Nucléaire (IRSN)
Laboratoire de Physique et de Métrologie des Aérosols (DSU/SERAC/LPMA)
Source :
Environmental Science and Technology, Environmental Science and Technology, American Chemical Society, 2013, 47 (19), pp.10995-11003. ⟨10.1021/es401973c⟩
Publication Year :
2013

Abstract

International audience; Segregation and radioactive analysis of aerosols according to their aerodynamic size were performed in France, Austria, the Czech Republic, Poland, Germany, and Greece after the arrival of contaminated air masses following the nuclear accident at the Fukushima Dai-ichi nuclear power plant in March 2011. On the whole and regardless of the location, the highest activity levels correspond either to the finest particle fraction or to the upper size class. Regarding anthropogenic radionuclides, the activity median aerodynamic diameter (AMAD) ranged between 0.25 and 0.71 μm for 137Cs, from 0.17 to 0.69 μm for 134Cs, and from 0.30 to 0.53 μm for 131I, thus in the "accumulation mode" of the ambient aerosol (0.1-1 μm). AMAD obtained for the naturally occurring radionuclides 7Be and 210Pb ranged from 0.20 to 0.53 μm and 0.29 to 0.52 μm, respectively. Regarding spatial variations, AMADs did not show large differences from place to place compared with what was observed concerning bulk airborne levels registered on the European scale. When air masses arrived in Europe, AMADs for 131I were about half those for cesium isotopes. Higher AMAD for cesium probably results from higher AMAD observed at the early stage of the accident in Japan. Lower AMAD for 131I can be explained by the adsorption of gaseous iodine on particles of all sizes met during transport, especially for small particles. Additionally, weathering conditions (rain) encountered during transport and in Europe in March and April contributed to the equilibrium of the gaseous to total 131I ratio. AMAD slightly increased with time for 131I whereas a clear decreasing trend was observed with the AMADs for 137Cs and 134Cs. On average, the associated geometric standard deviation (GSD) appeared to be higher for iodine than for cesium isotopes. These statements also bear out a gaseous 131I transfer on ambient particles of a broad size range during transport. Highest weighted activity levels were found on the 0.49-0.95 μm and on the 0.18-0.36 μm size ranges in France and in Poland, respectively. The contribution from resuspension of old deposited 137Cs was assessed for the coarse particle fractions only for the first sampling week. © 2013 American Chemical Society.

Details

ISSN :
15205851 and 0013936X
Volume :
47
Issue :
19
Database :
OpenAIRE
Journal :
Environmental sciencetechnology
Accession number :
edsair.doi.dedup.....1ce7a20b348ca10dbbc2db07ca00322b
Full Text :
https://doi.org/10.1021/es401973c⟩