Federal Research Centre the Subtropical Scientific Centre of the Russian Academy of Sciences, 2/28 Jānis Fabriciuss, Krasnodar Krai, Sochi, 354002, Russia.
Federal State Budgetary Institution "Caucasian State Biosphere Natural Reserve named after KH.G. Shaposhnikova, 8 Karl Marx Street, Krasnodar Krai, Sochi, Adler district, 354340, Russia.
J Environ Radioact. 2022 Oct;251-252:106952. doi: 10.1016/j.jenvrad.2022.106952. Epub 2022 Jul 4.
This paper reports on the radioecological properties of environmental components in the Mzymta and Sochi River valleys on the Russian Black Sea coast. The environmental components covered are river sediments, alluvial soils, mosses, and fluvial water. Inductively Coupled Plasma Mass Spectrometry (ICP-MS) was used to determine the distribution patterns of Th and U stemming from two geochemical alkaline barriers present in the river valleys. One is a calcium barrier resulting from the metamorphic transition from neutral mudstones to alkaline carbonate rocks. The other is a sodium barrier formed in estuaries under the influence of Na-rich tidal seawater. The sodium barrier was responsible for an increase in Th and U concentrations in river water, a slight decrease in soil and sediments, and strong sorption on mosses. The calcium barrier reduced Th and U concentrations in river water, but increased them in soil and mosses. In the Sochi River valley, the content of calcium in the components of the natural environment is higher compared to the Mzymta River valley and, on average, 4 times higher in the river water. This factor determines the relatively high Th and U content in the natural environment of the Sochi River valley, as these radionuclides are easily extracted from the mineral component of river water by carbonate solutions. On the whole, the radioecological status of the river valleys was recognized as favourable. Gamma radiation exposure dose rate near the surface (20-27 μR/h or less in mountainous areas and 9-17 μR/h in the lowlands) was below the natural level typical for open mountainous areas of central Russia. River sediments in both valleys had low radionuclide concentrations based on the specific activities of naturally occurring radionuclides Ra, Ra, Ra, Th, and K. In similar river basins that may be targeted for future development, accumulation of Th and U in soil and mosses on calcium barriers and elevated concentrations in river water on sodium barriers should be expected.
本论文报告了俄罗斯黑海沿岸姆济姆塔河和索契河流域环境成分的放射性生态学特性。所涵盖的环境成分包括河沉积物、冲积土、苔藓和河流水。电感耦合等离子体质谱法(ICP-MS)用于确定源自河谷中存在的两种地球化学碱性屏障的 Th 和 U 的分布模式。一个是钙屏障,源于从中性泥岩到碱性碳酸盐岩的变质过渡。另一个是在富钠潮汐海水影响下形成的河口钠屏障。钠屏障导致河水 Th 和 U 浓度增加,土壤和沉积物略有减少,对苔藓强烈吸附。钙屏障降低了河水 Th 和 U 的浓度,但增加了土壤和苔藓中的浓度。在索契河流域,与姆济姆塔河流域相比,自然环境成分中的钙含量较高,平均高出 4 倍河水。该因素决定了索契河流域自然环境中相对较高的 Th 和 U 含量,因为这些放射性核素很容易被碳酸盐溶液从河水中的矿物成分中提取出来。总的来说,河谷的放射性生态状况被认为是有利的。表面附近的伽马辐射暴露剂量率(山区为 20-27 μR/h 或以下,低地为 9-17 μR/h)低于俄罗斯中部开阔山区的自然水平。两个流域的河流沉积物基于天然放射性核素 Ra、Ra、Ra、Th 和 K 的比活度,具有较低的放射性核素浓度。在可能成为未来发展目标的类似河流流域中,预计钙屏障上的土壤和苔藓中 Th 和 U 的积累以及钠屏障上河水的浓度升高。