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Strontium-90 activity concentration in soil samples from the exclusion zone of the Fukushima daiichi nuclear power plant

机译:福岛第一核电站禁区的土壤样品中锶90的活动浓度

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摘要

The radioactive fission product 90Sr has a long biological half-life (˜18 y) in the human body. Due to its chemical similarity to calcium it accumulates in bones and irradiates the bone marrow, causing its high radio-toxicity. Assessing 90Sr is therefore extremely important in case of a nuclear disaster. In this work 16 soil samples were collected from the exclusion zone (<30 km) of the earthquake-damaged Fukushima Daiichi nuclear power plant, to measure 90Sr activity concentration using liquid scintillation counting. 137Cs activity concentration was also measured with gamma-spectroscopy in order to investigate correlation with 90Sr. The 90Sr activity concentrations ranged from 3.0 ± 0.3 to 23.3 ± 1.5 Bq kg−1 while the 137Cs from 0.7 ± 0.1 to 110.8 ± 0.3 kBq kg−1. The fact that radioactive contamination originated from the Fukushima nuclear accident was obvious due to the presence of 134Cs. However, 90Sr contamination was not confirmed in all samples although detectable amounts of 90Sr can be expected in Japanese soils, as a background, stemming from global fallout due to the atmospheric nuclear weapon tests. Correlation analysis between 90Sr and 137Cs activity concentrations provides a potentially powerful tool to discriminate background 90Sr level from its Fukushima contribution.
机译:放射性裂变产物 90 Sr在人体中具有较长的生物半衰期(〜18 y)。由于其与钙的化学相似性,它会积聚在骨骼中并照射骨髓,从而导致其高放射毒性。因此,在发生核灾难的情况下,评估 90 Sr非常重要。在这项工作中,从遭受地震破坏的福岛第一核电站的禁区(<30 km)收集了16个土壤样品,使用液体闪烁计数法测量了 90 Sr活性浓度。为了研究与 90 Sr的相关性,还用γ光谱法测量了 137 Cs的活性浓度。 90 Sr活性浓度范围从3.0±0.3到23.3±1.5 Bq kg -1 ,而 137 Cs从0.7±0.1到110.8± 0.3 kBq kg -1 。由于存在 134 Cs,因此放射性污染源于福岛核事故这一事实是显而易见的。但是,尽管在日本土壤中可以检测到 90 Sr的量作为背景,但由于所有大气中的全球沉降都可能导致 90 Sr污染,因此并未在所有样品中均确认到 90 Sr污染。核武器测试。 90 Sr和 137 Cs活性浓度之间的相关性分析提供了潜在的强大工具,可将背景 90 Sr的水平与福岛的贡献区分开。

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