Nageldinger G, Flowers A, Henry B, Postaük J
Kingston University, Applied Physics, Kingston upon Thames, Surrey.
Health Phys. 1998 Apr;74(4):472-7. doi: 10.1097/00004032-199804000-00009.
The uncertainty in gamma spectroscopic activity measurements is investigated for soil containing hot particles. A radioactivity inhomogeneity uncertainty needs to be taken into account, which depends on the density of hot particles in the sample geometry, the distribution of their activities, and the specific source-detector geometry. The maximum activity error due to hot particles in our sampled Chernobyl soil with a 137Cs activity of 100 kBq kg(-1) soil was 6% for our source detector geometry. The methodology presented might have a practical application in nuclear power plants to detect hot particles in a large quantity of dust or dirt. The number of hot particles present can be estimated if the activity of all particles is assumed to be similar. With this assumption 100 g of the investigated soil sample would contain about 500 hot particles with an approximate activity of 20 Bq each.
对含有热粒子的土壤中伽马能谱活度测量的不确定性进行了研究。需要考虑放射性不均匀性的不确定性,这取决于样品几何形状中热粒子的密度、它们的活度分布以及特定的源 - 探测器几何形状。对于我们采样的切尔诺贝利土壤,其中137Cs活度为100 kBq kg(-1)土壤,在我们的源探测器几何条件下,由热粒子引起的最大活度误差为6%。所提出的方法在核电站检测大量灰尘或污垢中的热粒子方面可能具有实际应用价值。如果假设所有粒子的活度相似,则可以估计存在的热粒子数量。基于此假设,100克被研究的土壤样品将包含约500个热粒子,每个热粒子的活度约为20 Bq。