Rääf C L, Hemdal B, Mattsson S
Department of Radiation Physics, Lund University, Malmö University Hospital, Sweden.
Health Phys. 2001 Oct;81(4):366-77. doi: 10.1097/00004032-200110000-00002.
From 1960 to 1980 and between 1987 and 1994 the whole-body content of 17Cs, and when possible also 134Cs, was measured in a group of subjects living in the city of Lund, Sweden (55.7 degrees N, 13.2 degrees E). The results have been analyzed to estimate the effective ecological half-time of fallout radiocesium in humans living in the area. The Lund area (The Province of Skåne) was subjected to a deposition of about 2 kBq m(-2) of pre-Chernobyl 137Cs from nuclear weapons testing and 1 kBq m(-2) of 137Cs from Chernobyl fallout in May 1986. The radiocesium from the nuclear weapons tests in the 1950's and 1960's still gave a significant contribution to the total 137Cs levels in humans in the post-Chernobyl study period (1987-1994) of about 0.4 Bq per kg body weight, which was about 10% of the peak post-Chernobyl concentration level of 137Cs (3.5-4 Bq kg(-1)) in 1987. The effective ecological half-time for 137Cs from Chernobyl was found to be 1.8 +/- 0.2 y. The aggregate transfer factor from deposition to mean activity concentration in man was estimated to be 3.6 Bq kg(-1)/kBq m(-2). These values may be compared with an effective ecological half-time of 1.3 y found in the reference group in the 1960's, and an aggregate transfer factor of 10 Bq kg(-1)/kBq m(-2). This difference is largely explained by the continuous nature of the global fallout leading to contamination on growing crops whereas the Chernobyl fallout occurred just prior to the South Swedish growing season, leading to less efficient transfer to crops and to human diet. The average committed individual effective dose (50 y) from ingested 137Cs from the Chernobyl fallout was estimated to be 0.02 mSv and from the nuclear weapons fallout (1945-1995) to be 0.20 mSv.
1960年至1980年以及1987年至1994年期间,对居住在瑞典隆德市(北纬55.7度,东经13.2度)的一组受试者测量了其体内的¹³⁷Cs含量,如有可能还测量了¹³⁴Cs含量。对测量结果进行了分析,以估算该地区居民体内沉降放射性铯的有效生态半衰期。隆德地区(斯科讷省)曾遭受过约2 kBq/m²的来自核武器试验的切尔诺贝利事故前¹³⁷Cs沉降,以及1986年5月1 kBq/m²的来自切尔诺贝利事故沉降的¹³⁷Cs。20世纪50年代和60年代核武器试验产生的放射性铯在切尔诺贝利事故后的研究期间(1987 - 1994年)对人体总¹³⁷Cs水平仍有显著贡献,约为每千克体重0.4 Bq,这约占1987年切尔诺贝利事故后¹³⁷Cs峰值浓度水平(3.5 - 4 Bq/kg)的10%。发现切尔诺贝利事故产生的¹³⁷Cs的有效生态半衰期为1.8±0.2年。从沉降到人体平均活度浓度的总转移系数估计为3.6 Bq/kg/kBq/m²。这些数值可与20世纪60年代在参考组中发现的1.3年的有效生态半衰期以及10 Bq/kg/kBq/m²的总转移系数相比较。这种差异主要是由于全球沉降的持续性导致生长作物受到污染,而切尔诺贝利事故沉降发生在瑞典南部生长季节之前,导致向作物和人类饮食的转移效率较低。切尔诺贝利事故沉降的摄入¹³⁷Cs所致的平均个人待积有效剂量(50年)估计为0.02 mSv,核武器沉降(1945 - 1995年)所致的为0.20 mSv。