埃列克特罗斯塔尔市受放射性污染地区采取净化措施后城市土壤的性质

D. N. Lipatov, V. A. Varachenkov, D. V. Manakhov, G. I. Agapkina, A. I. Shcheglov
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摘要

摘要 我们研究了城市中失效和轻微受损地区土壤上层的形态特性、pH值、有机碳含量以及137Cs和天然放射性核素(40K、226Ra、232Th)的比活度。研究于 2019 年在埃列克特罗斯塔尔市(莫斯科州)的城市生态系统中进行,即在辐射事件导致 137Cs 在当地沉淀 6 年之后。城市土壤上层的形态特征如下:棕灰色,轻粘土成分,小块状和块状结构,夹杂建筑垃圾和生活垃圾。在城市准地层和城市土壤的上层地层中,碳含量较低(低于 1%),且变异系数较大。在所研究的城市土壤中,水的 pH 值范围很广:从酸性(4.6-5.5)到高碱性(8.0)。相关分析表明,在 UR 的上层,有机碳含量减少,土壤环境碱化。在未采取净化措施的受污染城市生态系统的土壤剖面中,137Cs 呈累积型分布。经过净化的城市土壤剖面显示,137Cs 的比活度在地表层较低,而在埋藏的污染地层则达到最高值。在含有大量碎石的 UR 主体地层中,226Ra 的比活度有所增加。UR 和 TCH 的一些技术地层主要由石英砂组成,其 226Ra 和 40K 的比活度值非常低。城市土壤剖面中化学和辐射指标的相关性反映了挖掘和净化工作所形成的上层地层的不同成分和性质。
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Properties of Urban Soils after Decontamination Measures on the Radioactively Contaminated Territory of the City of Elektrostal

Abstract

We studied the morphological properties, pH, organic carbon content, and specific activity of 137Cs and natural radionuclides (40K, 226Ra, 232Th) in the upper horizons of soils in deactivated and slightly damaged areas of the city. The studies were carried out in the urban ecosystems of the city of Elektrostal (Moscow oblast) in 2019, i.e., 6 years after local precipitation of 137Cs due to a radiation incident. The morphological features of the upper horizons of urban soils were the following: brownish-gray color, light-loamy composition, and small-lumpy and lumpy structure, with inclusions of construction and household waste. In the upper horizons of urban quasizems and urban soils, a low carbon content (less than 1%) with high coefficients of variation were detected. In the studied urban soils, a wide range of water pH values was noted: from an acidic (4.6–5.5) to highly alkaline (>8.0) reaction. Correlation analysis showed that, in the upper horizons of UR, the content of organic carbon was reduced and alkalinization of the soil environment was observed. The accumulative type of distribution of 137Cs was recorded for soil profiles of polluted urban ecosystems in which decontamination measures were not carried out. The profiles of urban soils that were subjected to decontamination revealed low values of the specific activity of 137Cs in surface bulk layers and maxima in buried contaminated horizons. In the bulk horizons of UR, which include a large amount of crushed stone, there was an increase in the specific activity of 226Ra. Some technogenic horizons of UR and TCH, consisting mainly of quartz sand, are characterized by very low values of specific activities 226Ra and 40K. Correlations of chemical and radiation indicators in the profiles of urban soils reflect the different compositions and properties of upper horizons formed as a result of excavation and decontamination work.

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