Hölgye Z, Schlesingerová E, Tecl J, Filgas R
National Radiation Protection Institute, Srobárova 48, 100 00 Prague 10, Czech Republic.
J Environ Radioact. 2004;71(2):115-25. doi: 10.1016/S0265-931X(03)00162-0.
Forty-four soil samples were taken around the nuclear research centre Rez, near Prague. The mean activity concentrations of 238Pu, 239,240Pu, 241Am, 90Sr and 137Cs in uncultivated soil were 0.010, 0.26, 0.12, 2.7 and 23 Bq.kg(-1), respectively. Contents of radionuclides in cultivated soil were lower and in forest soil higher than in uncultivated soil. The mean activity ratios of 238Pu/239,240Pu, 241Am/239,240Pu, 90Sr/239,240Pu and 239,240Pu/137Cs in uncultivated soil were 0.041, 0.47, 10.9 and 0.013, respectively. The mean activity ratios in cultivated and forest soils were close to the values given above. It follows from the results that the source of 239,240Pu, 90Sr and 137Cs in the studied area is deposition from atmospheric nuclear tests, in the case of 137Cs also deposition from Chernobyl accident. The contribution of the research centre effluents was not proved for these radionuclides. Increased activity ratio of 241Am/239,240Pu indicates the presence of 241Am in the soils studied emanating from sources other than nuclear tests. Uniform distribution of the 241Am/239,240Pu activity ratio around the nuclear research centre and the absence of an area with evidently higher activity ratio, including at sites lying in the main wind direction, suggest that the additional activity of 241Am does not originate from the nuclear research centre. The additional source might be the deposition following the Chernobyl accident.
在布拉格附近的雷兹核研究中心周围采集了44个土壤样本。未开垦土壤中238Pu、239,240Pu、241Am、90Sr和137Cs的平均活度浓度分别为0.010、0.26、0.12、2.7和23 Bq.kg(-1)。耕种土壤中放射性核素的含量低于未开垦土壤,而森林土壤中的含量则高于未开垦土壤。未开垦土壤中238Pu/239,240Pu、241Am/239,240Pu、90Sr/239,240Pu和239,240Pu/137Cs的平均活度比分别为0.041、0.47、10.9和0.013。耕种土壤和森林土壤中的平均活度比接近上述值。结果表明,研究区域内239,240Pu、90Sr和137Cs的来源是大气核试验的沉降,就137Cs而言,还包括切尔诺贝利事故的沉降。对于这些放射性核素,未证实研究中心废水的贡献。241Am/239,240Pu活度比的增加表明,所研究土壤中存在源自核试验以外来源的241Am。241Am/239,240Pu活度比在核研究中心周围分布均匀,且不存在活度比明显更高的区域,包括位于主要风向的地点,这表明241Am的额外活度并非源自核研究中心。额外的来源可能是切尔诺贝利事故后的沉降。