Particle size distribution of radioactive aerosols after the Fukushima and the Chernobyl accidents
Jazyk angličtina Země Velká Británie, Anglie Médium print-electronic
Typ dokumentu časopisecké články, práce podpořená grantem
PubMed
23974074
DOI
10.1016/j.jenvrad.2013.07.016
PII: S0265-931X(13)00173-2
Knihovny.cz E-zdroje
- Klíčová slova
- AMAD, Aerosol size distribution, Chernobyl accident, Fukushima accident,
- MeSH
- černobylská havárie * MeSH
- havárie elektrárny Fukušima * MeSH
- monitorování radiace metody MeSH
- radioaktivní látky znečišťující vzduch analýza MeSH
- radioizotopy cesia analýza MeSH
- radioizotopy jodu analýza MeSH
- radionuklidy analýza MeSH
- ruthenium analýza MeSH
- velikost částic * MeSH
- zirkonium analýza MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Názvy látek
- radioaktivní látky znečišťující vzduch MeSH
- radioizotopy cesia MeSH
- radioizotopy jodu MeSH
- radionuklidy MeSH
- ruthenium MeSH
- zirkonium MeSH
Following the Fukushima accident, a series of aerosol samples were taken between 24th March and 13th April 2011 by cascade impactors in the Czech Republic to obtain the size distribution of (131)I, (134)Cs, (137)Cs, and (7)Be aerosols. All distributions could be considered monomodal. The arithmetic means of the activity median aerodynamic diameters (AMADs) for artificial radionuclides and for (7)Be were 0.43 and 0.41 μm with GDSs 3.6 and 3.0, respectively. The time course of the AMADs of (134)Cs, (137)Cs and (7)Be in the sampled period showed a slight decrease at a significance level of 0.05, whereas the AMAD pertaining to (131)I increased at a significance level of 0.1. Results obtained after the Fukushima accident were compared with results obtained after the Chernobyl accident. The radionuclides released during the Chernobyl accident for which we determined the AMAD fell into two categories: refractory radionuclides ((140)Ba, (140)La (141)Ce, (144)Ce, (95)Zr and (95)Nb) and volatile radionuclides ((134)Cs, (137)Cs, (103)Ru, (106)Ru, (131)I, and (132)Te). The AMAD of the refractory radionuclides was approximately 3 times higher than the AMAD of the volatile radionuclides; nevertheless, the size distributions for volatile radionuclides having a mean AMAD value of 0.51 μm were very close to the distributions after the Fukushima accident.
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