Matsuda Norihiro, Mikami Satoshi, Shimoura Susumu, Takahashi Junko, Nakano Masakazu, Shimada Kiyotaka, Uno Kiichiro, Hagiwara Shigetomo, Saito Kimiaki
Japan Atomic Energy Agency, 2-2-2 Uchisaiwai-cho, Chiyoda, Tokyo 100-8577, Japan.
Japan Atomic Energy Agency, 2-2-2 Uchisaiwai-cho, Chiyoda, Tokyo 100-8577, Japan.
J Environ Radioact. 2015 Jan;139:427-434. doi: 10.1016/j.jenvrad.2014.10.001. Epub 2014 Oct 28.
During the Fukushima Dai-ichi Nuclear Power Plant (NPP) accident, radioactive cesium was released in the environment and deposited on the soils. Depth profiles of radioactive cesium in contaminated soils provide useful information not only for radiation protection and decontamination operations but also for geoscience and radioecology studies. Soil samples were collected using a scraper plate three times between December 2011 and December 2012 at 84 or 85 locations within a 100-km radius of the Fukushima Dai-ichi NPP. In most of the obtained radioactive cesium depth profiles, it was possible to fit the concentration to a function of mass depth as either an exponential or hyperbolic secant function. By using those functions, following three parameters were estimated: (i) relaxation mass depth β (g cm(-2)), (ii) effective relaxation mass depth βeff (g cm(-2)), which is defined for a hyperbolic secant function as the relaxation mass depth of an equivalent exponential function giving the same air kerma rate at 1 m above the ground as the inventory, and (iii) 1/10 depth L1/10 (cm), at which the soil contains 90% of the inventory. The average β value (wet weight) including ones by hyperbolic secant function in December 2012, was 1.29 times higher than that in December 2011. In fact, it was observed that depth profiles at some study sites deviated from the typical exponential distributions over time. These results indicate the gradual downward migration of radioactive cesium in the soils. The L1/10 values in December 2012 were summarized and presented on a map surrounding the Fukushima Dai-ichi NPP, and the average value of L1/10 was 3.01 cm (n = 82) at this time. It was found that radioactive cesium remained within 5 cm of the ground surface at most study sites (71 sites). The sech function can also be used to estimate the downward migration rate V (kg m(-2) y(-1)). The V values in December 2012 (n = 25) were in good agreement with those found by a realistic approach using a diffusion and migration model. Almost all values ranged between 1.7 and 9.6 kg m(-2) y(-1) in this study.
在福岛第一核电站事故期间,放射性铯释放到环境中并沉积在土壤上。受污染土壤中放射性铯的深度分布不仅为辐射防护和去污作业提供了有用信息,也为地球科学和放射生态学研究提供了有用信息。在2011年12月至2012年12月期间,使用刮板在福岛第一核电站半径100公里范围内的84或85个地点采集了三次土壤样本。在大多数获得的放射性铯深度分布中,可以将浓度拟合为质量深度的函数,该函数可以是指数函数或双曲正割函数。通过使用这些函数,估计了以下三个参数:(i) 弛豫质量深度β(g cm⁻²),(ii) 有效弛豫质量深度βeff(g cm⁻²),对于双曲正割函数,它被定义为等效指数函数的弛豫质量深度,该等效指数函数在地面上方1米处给出与存量相同的空气比释动能率,以及(iii) 1/10深度L1/10(cm),即土壤中含有90%存量的深度。2012年12月包括双曲正割函数计算值在内的平均β值(湿重)比2011年12月高1.29倍。事实上,观察到一些研究地点的深度分布随时间偏离了典型的指数分布。这些结果表明放射性铯在土壤中逐渐向下迁移。总结了2012年12月的L1/10值并绘制在福岛第一核电站周围的地图上,此时L1/10的平均值为3.01厘米(n = 82)。发现在大多数研究地点(71个地点)放射性铯最多保留在地表以下5厘米处。双曲正割函数也可用于估计向下迁移速率V(kg m⁻² y⁻¹)。2012年12月的V值(n = 25)与使用扩散和迁移模型的实际方法得到的值高度一致。在本研究中,几乎所有值都在1.7至9.6 kg m⁻² y⁻¹之间。