Sahoo S K, Matsumoto M, Shiraishi K, Fujimoto K, Cuknic O, Zunic Z S
Department of Radiation Dosimetry, National Institute of Radiological Sciences, 4-9-1 Anagawa, Inage-ku, Chiba 263-8555, Japan.
Radiat Prot Dosimetry. 2007;127(1-4):407-10. doi: 10.1093/rpd/ncm294. Epub 2007 Jun 13.
The use of depleted uranium ammunition in South Serbia during the 1999 Kosovo conflict raised a great deal of public concern in the Balkans. Radioactivity levels of 238U in 20 wells and lake water samples were checked from the viewpoint of internal radiation exposure for South Serbian subjects. We have measured 238U concentration using inductively coupled plasma mass spectrometry, whereas thermal ionisation mass spectrometry has been used for the measurement of isotope ratios, e.g. 234U/238U and 235U/238U. The concentration of uranium in water samples varies in the range 1.37-63.18 mBq/L. 234U belongs to the 238U natural radioactive decay series, and at secular equilibrium, the abundance ratio, 234U/238U, corresponds to the ratio of their half-lives. The 234U/238U activity ratio varies in the range 0.88-2.2 and 235U/238U isotope ratio varies from 0.00698 to 0.00745. These findings indicate that uranium in water was a mixture of natural and anthropogenic origin. The annual effective dose due to 238U was estimated to be in the range 9.2 x 10(-5)-2.1 x 10(-3) mSv.
1999年科索沃冲突期间,在塞尔维亚南部使用贫铀弹药引发了巴尔干地区公众的广泛关注。从塞尔维亚南部居民受到内照射的角度,对20口水井和湖水样本中的238U放射性水平进行了检测。我们使用电感耦合等离子体质谱法测量了238U的浓度,而热电离质谱法则用于测量同位素比值,例如234U/238U和235U/238U。水样中铀的浓度在1.37 - 63.18 mBq/L范围内变化。234U属于238U天然放射性衰变系列,在长期平衡状态下,丰度比234U/238U与它们半衰期的比值相对应。234U/238U活度比在0.88 - 2.2范围内变化,235U/238U同位素比值在0.00698至0.00745之间变化。这些发现表明水中的铀是天然来源和人为来源的混合物。因238U导致的年有效剂量估计在9.2×10(-5) - 2.1×10(-3) mSv范围内。