Fukushima fallout at Milano, Italy
The radionuclides 131I, 137Cs and 134Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m−3 for 131I was recorded at...
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| Published in | Journal of environmental radioactivity Vol. 114; pp. 119 - 125 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
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England
Elsevier Ltd
01.12.2012
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| Abstract | The radionuclides 131I, 137Cs and 134Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m−3 for 131I was recorded at April 3–4, 2011. The first evidence of Fukushima fallout was confirmed with 131I and 137Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of 131I and 137Cs in the rainwater equal to 0.89 Bq L−1 and 0.12 Bq L−1, respectively. 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 was more effective in the case of 137Cs than it was for 131I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of 137Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern.
► Radioactive plume from Fukushima reactor accident reached Milano, Italy. ► 131I, 137Cs and 134Cs were determined in rainwater, air, soil, grass and milk samples. ► The 134Cs/137Cs activity ratio values in air was about 1. ► High observed values of 137Cs in grass, soil and milk samples are not due to Fukushima accident. ► The dose assessment show that the observed activities are very far below levels of concern. |
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| AbstractList | The radionuclides (131)I, (137)Cs and (134)Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m(-3) for (131)I was recorded at April 3-4, 2011. The first evidence of Fukushima fallout was confirmed with (131)I and (137)Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of (131)I and (137)Cs in the rainwater equal to 0.89 Bq L(-1) and 0.12 Bq L(-1), respectively. 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 was more effective in the case of (137)Cs than it was for (131)I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of (137)Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern.The radionuclides (131)I, (137)Cs and (134)Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m(-3) for (131)I was recorded at April 3-4, 2011. The first evidence of Fukushima fallout was confirmed with (131)I and (137)Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of (131)I and (137)Cs in the rainwater equal to 0.89 Bq L(-1) and 0.12 Bq L(-1), respectively. 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 was more effective in the case of (137)Cs than it was for (131)I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of (137)Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern. The radionuclides 131I, 137Cs and 134Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m−3 for 131I was recorded at April 3–4, 2011. The first evidence of Fukushima fallout was confirmed with 131I and 137Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of 131I and 137Cs in the rainwater equal to 0.89 Bq L−1 and 0.12 Bq L−1, respectively. 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 was more effective in the case of 137Cs than it was for 131I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of 137Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern. ► Radioactive plume from Fukushima reactor accident reached Milano, Italy. ► 131I, 137Cs and 134Cs were determined in rainwater, air, soil, grass and milk samples. ► The 134Cs/137Cs activity ratio values in air was about 1. ► High observed values of 137Cs in grass, soil and milk samples are not due to Fukushima accident. ► The dose assessment show that the observed activities are very far below levels of concern. The radionuclides ¹³¹I, ¹³⁷Cs and ¹³⁴Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m⁻³ for ¹³¹I was recorded at April 3–4, 2011. The first evidence of Fukushima fallout was confirmed with ¹³¹I and ¹³⁷Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of ¹³¹I and ¹³⁷Cs in the rainwater equal to 0.89 Bq L⁻¹ and 0.12 Bq L⁻¹, respectively. 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 was more effective in the case of ¹³⁷Cs than it was for ¹³¹I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of ¹³⁷Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern. The radionuclides ¹³¹I, ¹³⁷Cs and ¹³⁴Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m⁻³ for ¹³¹I was recorded at April 3–4, 2011. The first evidence of Fukushima fallout was confirmed with ¹³¹I and ¹³⁷Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of ¹³¹I and ¹³⁷Cs in the rainwater equal to 0.89 Bq L⁻¹ and 0.12 Bq L⁻¹, respectively. 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 was more effective in the case of ¹³⁷Cs than it was for ¹³¹I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of ¹³⁷Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern. The radionuclides (131)I, (137)Cs and (134)Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 μBq m(-3) for (131)I was recorded at April 3-4, 2011. The first evidence of Fukushima fallout was confirmed with (131)I and (137)Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of (131)I and (137)Cs in the rainwater equal to 0.89 Bq L(-1) and 0.12 Bq L(-1), respectively. 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 was more effective in the case of (137)Cs than it was for (131)I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of (137)Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern. The radionuclides 131I, 137Cs and 134Cs were observed in the Milano region (45 degree ) of Italy early after the nuclear accident in Fukushima, Japan. Increased atmospheric radioactivity was observed on an air filter taken on 30 March 2011, while the maximum activity of 467 mu Bq m-3 for 131I was recorded at April 3-4, 2011. The first evidence of Fukushima fallout was confirmed with 131I and 137Cs measured in precipitation at two sampling sites at Milano on 28 March, 2011, with the concentrations of 131I and 137Cs in the rainwater equal to 0.89 Bq L-1 and 0.12 Bq L-1, respectively. 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 was more effective in the case of 137Cs than it was for 131I, probably because iodine was mainly in gaseous form whereas caesium was rapidly bound to aerosols and thus highly subject to dry deposition. The relatively high observed values of 137Cs in grass, soil and fresh goat and cow milk samples were probably from Chernobyl fallout and global fallout from past nuclear tests rather than from the Fukushima accident. Finally, a dose assessment for the region of investigation showed clearly that the detected activities in all environmental samples were very far below levels of concern. |
| Author | Luigi Gini Ioannidou, Alexandra Manenti, Simone Groppi, Flavia |
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| Keywords | Radioactive nuclides Fukushima accident Radioactive fallout Nuclear accident |
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| Snippet | The radionuclides 131I, 137Cs and 134Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased... The radionuclides ¹³¹I, ¹³⁷Cs and ¹³⁴Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased... The radionuclides (131)I, (137)Cs and (134)Cs were observed in the Milano region (45°) of Italy early after the nuclear accident in Fukushima, Japan. Increased... The radionuclides 131I, 137Cs and 134Cs were observed in the Milano region (45 degree ) of Italy early after the nuclear accident in Fukushima, Japan.... |
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| SubjectTerms | Adult aerosols air analysis Animals Assessments cesium Cesium Radioisotopes Cesium Radioisotopes - analysis chemistry Deposition dry deposition Drying Fallout Food Contamination, Radioactive Food Contamination, Radioactive - analysis Fukushima accident Fukushima Nuclear Accident Goats grasses Humans Infant iodine Iodine Radioisotopes Iodine Radioisotopes - analysis Italy Japan Milk Milk - chemistry Nuclear accident Nuclear accidents Poaceae Poaceae - chemistry Radiation Dosage Radiation Monitoring Radioactive fallout Radioactive nuclides Radioactive Pollutants Radioactive Pollutants - analysis Radioactivity radionuclides rain Rain - chemistry Risk Assessment Snow Snow - chemistry soil Soil - analysis |
| Title | Fukushima fallout at Milano, Italy |
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