{"title":"Fukushima fallout of 131I, 137Cs, 134Cs at Milano, Italy","authors":"A. Ioannidou, S. Manenti, L. Gini, F. Groppi","doi":"10.1109/ICNC.2011.6022595","DOIUrl":null,"url":null,"abstract":"<sup>131</sup>I and <sup>137</sup>Cs and <sup>134</sup>Cs fallout isotopes were measured in the Milano region (45°N), Italy over one month after the nuclear accident in Fukushima, Japan. Daily monitoring of the airborne activity levels carried out with a high volume air sampler, gave increased atmospheric radioactivity on air filter taken on 30 March 2011, while the maximum activity of 467 µBq m<sup>−3</sup>, occurred at April 3–4, 2011. Radionuclides from Fukushima fallout were first detected at Milano region in a rain water sample, at 27–28 March, 2011 with the concentrations of <sup>131</sup>I and <sup>137</sup>Cs isotopes in the rainwater to be equal to 0.89 Bq L<sup>−1</sup> and 0.12 Bq L<sup>−1</sup>, respectively. During the same days a snowfall sample was collected from Monte Rosa mountain at a height of 3000 m, with the concentrations of <sup>131</sup>I and <sup>137</sup>Cs in snowfall to be lower than that in rainwater sample. A sample of dry deposition that was collected 9 days after the first rainfall event of 27-28 March, 2011 showed that the dry deposition of <sup>131</sup>I and <sup>137</sup>Cs was 0.40 Bq m<sup>−2</sup> and 0.24 Bq m<sup>−2</sup> respectively. The concentration of <sup>131</sup>I in goat and cow milk samples collected on 9 April, 2011 from a farm at a village in Anzasca valley near Macugnaga (Monte Rosa mountain), were 0.30 Bq L<sup>−1</sup> and 0.37 Bq L<sup>−1</sup> respectively.","PeriodicalId":299503,"journal":{"name":"2011 Seventh International Conference on Natural Computation","volume":"45 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2011-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2011 Seventh International Conference on Natural Computation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ICNC.2011.6022595","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3
Abstract
131I and 137Cs and 134Cs fallout isotopes were measured in the Milano region (45°N), Italy over one month after the nuclear accident in Fukushima, Japan. Daily monitoring of the airborne activity levels carried out with a high volume air sampler, gave increased atmospheric radioactivity on air filter taken on 30 March 2011, while the maximum activity of 467 µBq m−3, occurred at April 3–4, 2011. Radionuclides from Fukushima fallout were first detected at Milano region in a rain water sample, at 27–28 March, 2011 with the concentrations of 131I and 137Cs isotopes in the rainwater to be equal to 0.89 Bq L−1 and 0.12 Bq L−1, respectively. During the same days a snowfall sample was collected from Monte Rosa mountain at a height of 3000 m, with the concentrations of 131I and 137Cs in snowfall to be lower than that in rainwater sample. A sample of dry deposition that was collected 9 days after the first rainfall event of 27-28 March, 2011 showed that the dry deposition of 131I and 137Cs was 0.40 Bq m−2 and 0.24 Bq m−2 respectively. The concentration of 131I in goat and cow milk samples collected on 9 April, 2011 from a farm at a village in Anzasca valley near Macugnaga (Monte Rosa mountain), were 0.30 Bq L−1 and 0.37 Bq L−1 respectively.