Ishida Masanobu, Yamazaki Hideo
Graduate School of Science and Engineering, Kindai University, Higashiosaka, Osaka, Japan.
PLoS One. 2017 Nov 14;12(11):e0187687. doi: 10.1371/journal.pone.0187687. eCollection 2017.
Radioactive contamination in the Tokyo metropolitan area in the immediate aftermath of the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident was analyzed via surface soil sampled during a two-month period after the accident. 131I, 134Cs, and 137Cs were detected in these soil samples. The activity and inventory of radioactive material in the eastern part of Tokyo tended to be high. The 134Cs/137Cs activity ratio in soil was 0.978 ± 0.053. The 131I/137Cs ratio fluctuated widely, and was 19.7 ± 9.0 (weighted average 18.71 ± 0.13, n = 14) in the Tokyo metropolitan area. The radioactive plume with high 131I activity spread into the Tokyo metropolitan area and was higher than the weighted average of 6.07 ± 0.04 (n = 26) in other areas. The radiocesium activity and inventory surveyed in soil from a garden in Chiyoda Ward in the center of Tokyo, fell approximately 85% in the four months after the accident, and subsequently tended to rise slightly while fluctuating widely. It is possible that migration and redistribution of radiocesium occurred. The behavior of radiocesium in Tokyo was analyzed via monitoring of radiocesium in sludge incineration ash. The radiocesium activity in the incineration ash was high at wastewater treatment centers that had catchment areas in eastern Tokyo and low at those with catchment areas in western Tokyo. Similar to the case of the garden soil, even in incineration ash, the radiocesium activity dropped rapidly immediately after the accident. The radiocesium activity in the incineration ash fell steadily from the tenth month after the accident until December 2016, and its half-life was about 500 days. According to frequency analysis, in central Tokyo, the cycles of fluctuation of radiocesium activity in incineration ash and rainfall conformed, clearly showing that radiocesium deposited in urban areas was resuspended and transported by rainfall run-off.
通过分析福岛第一核电站事故发生后两个月内采集的表层土壤样本,对东京都市区的放射性污染情况进行了研究。在这些土壤样本中检测到了¹³¹I、¹³⁴Cs和¹³⁷Cs。东京东部地区放射性物质的活度和总量往往较高。土壤中¹³⁴Cs/¹³⁷Cs活度比为0.978±0.053。¹³¹I/¹³⁷Cs比值波动较大,在东京都市区为19.7±9.0(加权平均值18.71±0.13,n = 14)。¹³¹I活度较高的放射性烟羽扩散到东京都市区,高于其他地区6.07±0.04(n = 26)的加权平均值。对东京市中心千代田区一个花园土壤中放射性铯的活度和总量进行调查,结果显示事故发生后的四个月内下降了约85%,随后虽有波动但略有上升趋势。放射性铯可能发生了迁移和重新分布。通过监测污泥焚烧灰中的放射性铯,分析了东京放射性铯的行为。在东京东部集水区的污水处理中心,焚烧灰中的放射性铯活度较高,而在东京西部集水区的污水处理中心则较低。与花园土壤情况类似,即使在焚烧灰中,事故发生后放射性铯活度也迅速下降。焚烧灰中的放射性铯活度从事故发生后的第十个月到2016年12月稳步下降,其半衰期约为500天。频率分析表明,在东京市中心,焚烧灰中放射性铯活度的波动周期与降雨情况相符,清楚地表明城市地区沉积的放射性铯会因降雨径流而重新悬浮和迁移。