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The sources and fate of 210Po in the urban air: A review
Affiliation:1. College of Resource and Environment, Qingdao Agricultural University, Qingdao, 266109, Shandong, China;2. College of Biological Sciences and Technology, Beijing Forestry University, Beijing 100083, China;1. Environment and Life Sciences Research Center, Kuwait Institute for Scientific Research, Kuwait;2. Institute Bobby, 8 Allée des Orangers, 06320 Cap d''Ail, France;3. International Atomic Energy Agency, Environment Laboratories, 4a, Quai Antoine 1er, MC-98000, Monaco;1. Department of Biology, Faculty of Science, Istanbul University, 34134, Vezneciler, Istanbul, Turkey;2. Institute of Graduate Studies in Sciences, Istanbul University, Suleymaniye, Istanbul, Turkey;3. Gökçeada Marine Research Department, Istanbul University, 17100, Çanakkale, Turkey;4. Institute of Marine Science and Management, Istanbul University, 34134, Vezneciler, Istanbul, Turkey;1. Centre for Advanced Research in Environmental Radioactivity, Mangalore University, Mangalagangothri, 574 199, India;2. Department of Chemical Engineering, Indian Institute of Technology-Bombay, Mumbai, 400 076, India;1. Institute of Radiochemistry and Radioecology, University of Pannonia, 10 Egyetem str., H-8200, Veszprém, Hungary;2. Social Organisation for Radioecological Cleanliness, 7/a József Attila str., H-8200, Veszprém, Hungary;1. Centre for Advanced Research in Environmental Radioactivity, Mangalore University, Mangalagangotri, 574 199, India;2. Department of Chemical Engineering, Indian Institute of Technology-Bombay, Mumbai, 400 076, India
Abstract:
The origin of 210Po activity and its fluctuations in the air are discussed in this paper. In the case of atmospheric aerosol samples, a comparison of the 210Po/210Pb and 210Bi/210Pb activity ratios makes it possible not only to determine aerosol residence times but also to appraise the contribution of the unsupported 210Po coming from other sources than 222Rn decay, such as human industrial activities, especially coal combustion. A simple mathematical method makes it possible to observe the seasonal fluctuations of the anthropogenic excess of 210Po in the urban air. The average doses of 210Po intake with food (including drinking water) and inhalation of urban aerosols are usually lower than those from 210Po intake by cigarette smokers and negligible in comparison to total natural radiation exposure.
Keywords:
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