Assessment of plutonium isotopes content in soil at the vicinity of the radioactive waste storage facility in Obninsk

M. A. Edomskaya, S. Lukashenko, A. A. Shupik, S. V. Korovin, A. V. Tomson
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Abstract

One of the sources of radionuclides released into the environment are radioactive waste storage. The plutonium isotopes concentration in the soils of the territory adjacent to the former radioactive waste storage facility in Obninsk was estimated. The cause of pollution was the depressurization of one of the storage tanks and the release of radionuclides due to its overflow with surface and ground waters in the period from 1998 to 1999. Samples were analyzed by alpha spectrometry with preliminary radiochemical isolation with complete decomposition of soil samples. The Pu-239+240 content range in the surface soil layer was 3.7-9.6 Bq/kg, with an average value of 6.7 Bq/kg, which is an order of magnitude higher than the level of its global fallout. In some samples, significant amounts of Pu-238 are observed, the relative content of which is 10-50% of Pu-239+240, that exceeds the its relative content due to the global fallout which is 2-5%. The depth distribution of plutonium isotopes has been studied. It has been established those significant concentrations of plutonium are observed to the depth of 95 cm for this territory. There is no definite dependence of the distribution of plutonium isotopes along the vertical soil profile. The random distribution of plutonium to the soil depth indicates that the source of Pu-239+240 are groundwater. Elevated concentrations of plutonium isotopes in the soil surface of the territory under consideration, its significant concentrations at soil depth indicates that the contamination is a consequence of the leakage of plutonium isotopes from the radioactive waste storage facility in Obninsk. The same concentrations can be expected in the lowland of the adjacent territory.
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奥布宁斯克放射性废物储存设施附近土壤中钚同位素含量的评估
放射性核素释放到环境中的来源之一是放射性废物储存。对奥布宁斯克前放射性废物储存设施附近领土土壤中的钚同位素浓度进行了估计。污染的原因是1998年至1999年期间,其中一个储罐的降压和由于地表水和地下水溢出而释放的放射性核素。样品采用初步放射化学分离的α光谱法进行分析,土壤样品完全分解。表层土壤中Pu-239+240含量范围为3.7 ~ 9.6 Bq/kg,平均值为6.7 Bq/kg,高于其全球沉降水平一个数量级。在一些样品中,观察到大量的Pu-238,其相对含量为Pu-239+240的10-50%,超过了由于全球沉降而导致的2-5%的相对含量。对钚同位素的深度分布进行了研究。已经确定,在该领土95厘米深处观察到钚的显著浓度。钚同位素沿垂直土壤剖面的分布没有明确的依赖性。钚在土壤深度上的随机分布表明,钚239+240的来源是地下水。所审议领土土壤表面的钚同位素浓度升高,土壤深处的钚同位素浓度很高,这表明污染是奥布宁斯克放射性废物储存设施泄漏钚同位素的结果。预计在邻近地区的低地也会有同样的浓度。
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