Variation in airborne 134Cs, 137Cs, particulate 131I and 7Be maximum activities at high-altitude European locations after the arrival of Fukushima-labeled air masses
Creators
- 1. Institut de Radioprotection et de Sûreté Nucléaire (IRSN), BP 3, 13115, St Paul lez Durance, Cedex (France)
- 2. Bundesamt für Strahlenschutz (BfS), 79098 Freiburg (Germany)
- 3. Laboratorio di Chimica e Radioattività ambientale, University of Bologna, 40126 Bologna (Italy)
- 4. Deutscher Wetterdienst (DWD), Referat TI 24, Frankfurterstraße 135, 63067 Offenbach (Germany)
- 5. Federal Office of Public Health, (FOPH), Schwarzenburgstrasse 165, CH-3003 Bern (Switzerland)
- 6. Institute for Nuclear Research and Nuclear Energy (INRNE), 72 Tzarigradsko shosse, Blvd Bulgarian Academy of Sciences, 1784 Sofia (Bulgaria)
- 7. Austrian Agency for Health and Food Safety (AGES), Radon and Radioecology, 4020 Linz (Austria)
- 8. Laboratoire d'Etudes en Géophysique et Océanographie Spatiales (LEGOS), Observatoire Midi Pyrénées, 14 avenue Edouard Belin, 31400 Toulouse (France)
Description
The Fukushima-labeled air mass arrival, and later the cesium-134 (134Cs), cesium-137 (137Cs) and particulate iodine-131 (hereafter noted 131Ip) maximum levels were registered in Europe at different dates depending on the location. Most of those data were obtained at low-altitude sampling areas. Here, we compare the airborne levels registered at different high-altitude European locations (from 850 m to about 3500 m). The integrated 137Cs activity concentration was not uniform with regard to the altitude even after a long travel time/distance from Japan. Moreover, the relation of integrated 137Cs vs. altitude showed a linear decrease up to an altitude of about 3000 m. A similar trend was noticed for 131Ip (particulate fraction) while it increased above 3000 m. Comparison with 7Be activity concentration showed that, as far as the high altitude location is concerned, the 137Cs and 134Cs maximum concentrations corresponded to the 7Be maximum, suggesting downdraft movements from high tropospheric or stratospheric layers to be responsible for 137,134Cs increase and peak values. This was also confirmed by high potential vorticity and low relative humidity registered during the peak values. - Highlights: • Airborne radionuclides from the FDNPP accident, at high-altitude locations across Europe. • Total amount of 137Cs that passed was not homogeneous with regard to the altitude. • Peak concentrations were due to downdrafts as revealed by 7Be maximum and potential vorticity. • In accident situation, gaseous 131I monitoring should be more widely performed as for aerosols.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.jenvrad.2016.05.004Additional details
Identifiers
- DOI
- 10.1016/j.jenvrad.2016.05.004;
- PII
- S0265-931X(16)30148-5;
Publishing Information
- Journal Title
- Journal of Environmental Radioactivity
- Journal Volume
- 162-163
- Journal Page Range
- p. 14-22
- ISSN
- 0265-931X
- CODEN
- JERAEE
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 49055930
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AIR POLLUTION; ALTITUDE; BERYLLIUM 7; CESIUM 134; CESIUM 137; COMPARATIVE EVALUATIONS; CONCENTRATION RATIO; ECOLOGICAL CONCENTRATION; FUKUSHIMA DAIICHI NUCLEAR POWER STATION; IODINE 131; JAPAN; MASS; PARTICULATES; PEAKS; REACTOR ACCIDENTS
- Descriptors DEC
- ACCIDENTS; ALKALINE EARTH ISOTOPES; ASIA; BERYLLIUM ISOTOPES; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; CESIUM ISOTOPES; DAYS LIVING RADIOISOTOPES; DEVELOPED COUNTRIES; DIMENSIONLESS NUMBERS; ELECTRON CAPTURE RADIOISOTOPES; EVALUATION; EVEN-ODD NUCLEI; HOURS LIVING RADIOISOTOPES; INTERMEDIATE MASS NUCLEI; INTERNAL CONVERSION RADIOISOTOPES; IODINE ISOTOPES; ISOMERIC TRANSITION ISOTOPES; ISOTOPES; LIGHT NUCLEI; NUCLEI; ODD-EVEN NUCLEI; ODD-ODD NUCLEI; PARTICLES; POLLUTION; RADIOISOTOPES; REACTOR SITES; YEARS LIVING RADIOISOTOPES
Optional Information
- Copyright
- Copyright (c) 2016 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.