Alexey Ivanovich Shcheglov

The possibility of using algorithm VERT_MIG the simulations of vertical migration of radionuclides in the soil are discussed. The algorithm was successfully used to develop models of migration 137Cs and 90Sr in radioactive contamination of different soils as a result of accidents at Chernobyl and Fukushima-1. The results of modeling are presented. The prospects for further use of this algorithm and some aspects of the use of simulation in this area are discussed.

The article is dedicated to the analysis of content and distribution of oil hydrocarbons in the soils of geochemical landscapes of the southern Sakhalin. It is discussed the main types of soil formed in this region, and the parameters determining the migration of oil hydrocarbons in the landscapes. It was shown that the soils of transit-accumulative and accumulative landscapes are characterized by the highest content and the depth of oil hydrocarbons penetration into the soil profile. In the case of accidental oil spills, along with lateral migration significant role will play vertical migration of oil hydrocarbons to the accumulative landscapes.

The ²²⁶Ra, ²³²Th, ⁴⁰K vertical profiles were studied in relation with the soil properties: pH_H2O, the sum of exchangeable Ca²⁺ and Mg²⁺, the degree of saturation with bases, the content of humus, mobile forms of phosphorus and potassium. An increase in the specific activity of ²²⁶Ra, ²³²Th, ⁴⁰K associated with the accumulation of humus and the biogenic accumulation of mobile forms of potassium and phosphorus in the upper 0-10 cm layer of horizon A in the soil of the oak forest was detected. The removal of ²²⁶Ra from the middle part of the profile of dark gray forest deep-carbonate soil was recorded. A positive correlation between the specific activity of ²²⁶Ra and the sum of the exchange bases Ca²⁺ and Mg²⁺ indicating the conjugate behavior of these elements-analogues in the horizons A, A(AE), AB and the lower horizons B1, B2, B3 was revealed. Removal of ²³²Th from horizon A(AE) and accumulation in horizon AB under conditions of local podzolization of dark gray forest soil in birch forest was observed.

Some aspects of application of simulation modeling of radionuclide behavior in food chains of terrestrial ecosystems are discussed. The model of behavior of ¹³⁷Cs in the system of type soil-vegetation-herbivores-predators is described. The results of modeling, including the calculation of the dynamics of dose load on animals, are presented. It is shown that in the simplified “Chernobyl” scenario of the radiological situation, dose loads on herbivores are significantly lower than on predators. In general, in animals in the first 10 years, the main contribution to the dose load is made by external irradiation. Then the external and internal dose loads become approximately equal.

The features of the modern radioecological situation in forest (pine, spruce, birch) and fallow ecosystems in the contaminated (southern part) and background (northern part) territories of the Kaluga region are analyzed in this article. The density of soil contamination of the studied region by natural radionuclides (²²⁶Ra, ²³²Th, ⁴⁰K) corresponds to background levels, while technogenic radionuclide (¹³⁷Cs) significantly exceeds the background value (3 kBq/m²) and ranges from 60,8 to 273,8 kBq/m². Forest ecosystems (especially coniferous) are the most contaminated by ¹³⁷Cs, and fallow ones are the least contaminated. The density of ¹³⁷Cs soil contamination has decreased on average by more than 3 times compared to the initial period after fallouts (1986), but still significantly exceeds the permissible level (37 kBq/m²). The main contribution to the total specific activity of soils, as well as the power of the equivalent absorbed dose, is made by ¹³⁷Cs in the ecosystems of the contaminated areas, and by ⁴⁰K - in the ecosystems of background areas.

The simulation model of seasonal dynamics of ¹³⁷Cs in the components of the snytevoy oak forest ecosystem EcoradOak_CS_FW was further developed, which now includes first- and second-order consumers. The radiocesium redistribution in a full-scale food web of   a forest ecosystem of the type “soil—vegetation cover—herbivores—predators” is modeled. The algorithm used in the model allows us to take into account the influence of soil, meteorological, phenological and physiological factors on the behavior of radionuclide in the food web and predict radiological situations under various conditions of radioactive fallout. Data   on the contamination of animals with radiocesium obtained using the model are used to calculate the dynamics of the internal dose. The results of modeling can be used in the rationing of forest products of deciduous forests. The model is also applicable to the study of potassium redistribution in the trophic chain of a deciduous forest ecosystem.

The article provides an overview of the results of long-term studies of the migration of radionuclides in the composition of lysimetric waters. The features of lysimetric studies at various stages of radioecology development are considered. It is noted that the use of lysimeters for a long time was limited to low levels of radionuclides in soil solutions, and large-scale studies began after the Chernobyl fallout (1986). It is shown that the greatest output of radionuclides in lysimetric waters occurs in forest, especially coniferous phytocenoses, the least — in meadow and agrophytocenoses. In the long-term dynamics, the maximum intensity of radionuclide migration in the lysimetric waters is observed in the initial period after aerial precipitation, in the seasonal period — in the summer. A small amount of radionuclides migrates with downward water flow. Annual outflow with vertical subsurface runoff varies depending on soil-climatic conditions, the period after precipitation, the thickness and depth of the layer. Annual outflow from the forest litter layer varies from tenths to units of percentage, from the layer 0–20 cm — from hundredths to tenths of a percentage from the total radionuclide supply in these layers. The relative output of ⁹⁰Sr is much bigger than ¹³⁷Cs. In soil solution from 70% to 90% radionuclides [¹⁴⁴Ce, ²³⁹Pu ¹⁰⁶Ru ,¹³⁷Cs and ⁹⁰Sr] are in the form of radionuclide-organic compounds of various molecular weights. 

The aim of the work is to summarize the data available in the scientific literature on the values of the ¹³⁷Cs/¹³³Cs isotope ratio in soils and vegetation cover of forest ecosystems in radioactively contaminated and background territories. The values of the specific activity of ¹³⁷Cs and the concentration of ¹³³Cs presented in radioecological studies are unified by calculating the molar ratio of these isotopes. Based on the generalized literature data, it is shown that the values of ¹³⁷Cs/¹³³Cs in soils, forest litter and vegetation increase in radioactively contaminated areas. In background regions exposed only to global radioactive fallout, the isotopic ratio of ¹³⁷Cs/¹³³Cs is about 0,1–1,0 (× 10^-8), whereas in the Chernobyl fallout zone it increases by 1000–100 000 times. The isotopic ratio of ¹³⁷Cs/¹³³Cs decreases down the soil profiles in various forest ecosystems. Spatial variation of the ¹³⁷Cs/¹³³Cs ratio in litter is associated with the diversity of ecotopes in forest biogeocenoses. The alignment of the values of the ¹³⁷Cs/¹³³Cs ratio in the vegetation cover and upper soil horizons indicates the achieved equilibrium of technogenic ¹³⁷Cs with natural stable ¹³³Cs in the biogeochemical cycle of this element. A comparative study revealed that the isotopic ratio of ¹³⁷Cs/¹³³Cs increases in the following range of plant cover representatives: Bryophyta < Sorbus aucuparia < Lichenes < Russula vesca < Frangula alnus < Polypodiophyta. For fungi, interspecific differences were noted in the following increasing series in the isotopic ratio ¹³⁷Cs/¹³³Cs: Lactarius deliciosus < Sarcodon scabrosus < Suillus bovinus < Tricholoma saponaceum < Lepista nuda < Russula delica < Macrolepiota excoriata. For the reference species of coniferous trees — Pinus sylvestris - the isotopic ratio of ¹³⁷Cs/¹³³Cs in the forest area of the Bryansk region polluted by Chernobyl fallout increases in the following number of components: roots < large branches < trunk wood < needles < small branches < cones.

The study of ¹³⁷Cs and K behavior in «soil-plant» system of chernozem zone in remote period after Chernobyl accident was carried out. Experimental plots in agrosystems such as wheat, soybean, buckwheat, rapeseed, sunflower, grass mixture, and natural biosystem of a dry meadow were selected in the central part of Plavsk radioactive hotspot in Tula region. The level of ¹³⁷Cs soil contamination was 171 ± 26 kBq/m² (498 ± 100 Bq/kg). Average gross K content in soils was 2,0 ± 0,1%, including exchangeable K — 235 ± 54 mg/kg and non–exchangeable K — 816 ± 116 mg/kg. Vertical distribution of ¹³⁷Cs within contaminated 30-cm soil layer of agrosystems, as well as gross K, was uniformly accumulative, while K_ex and K_non-ex distribution was regressive and accumulative. At the same time, ¹³⁷Cs microdistribution in root zone was invariant, and gradient enrichment of soil near the root surface was shown for mobile forms of potassium. Intensity of ¹³⁷Cs transfer from soils to plants for all studied crops was 1–2 orders lower than intensity of K root uptake. Element distribution between plant organs differed. ¹³⁷Cs distribution was acropetal for Cereals and basipetal for crops from other families, and K was distributed basipetally in all tested plants.

The article discusses the processes of transition to the aqueous phase and uptake from it by plants of stable (Cd) and radioactive (¹⁰⁹Cd) isotopes. Regularities of the distribution of Cd/¹⁰⁹Cd between different forms of their chemical compounds in the soil were revealed by means of sequental extraction procedure (SEP) according to the Tessier-Förstner method. It was shown that content of labile and conditionally labile forms of compounds (fraction F1-F3) of stable Cd was 1,2–1,8 times less than that of radioactive ¹⁰⁹Cd and, conversely, 2,4–5,3 times more fixed conservative forms of metal compounds (fraction F4-F6). The Cd concentration, ¹⁰⁹Cd activity concentration, distribution and concentration coefficients of natural Cd and ¹⁰⁹Cd radionuclide, accumulation and removal of metal by plants were evaluated. Values of enrichment coefficients of natural (stable) Cd contained in sequentially extracted chemical fractions by ¹⁰⁹Cd radioisotope were determined, the value of stock of labile cadmium compounds in studied soil was calculated. Based on the results of solid-state ¹³C NMR spectrometry, the qualitative composition of high-molecular organic compounds of the soil solution was determined and their ability to specifically sorb heavy metal cations was assessed.

The article deals with issues related to the development of radioecology as an independent scientific discipline. The achievements of the past years, the studies that are currently being carried out, as well as promising areas of development in this area are analyzed. A corrected periodization of the stages of development of radioecology is proposed, taking into account the experience accumulated to date in the field of this discipline. At the initial stage (1895–1929:), empirical material was collected; at the first stage (1930–1960), the theoretical foundation was laid and radioecology was formed as an independent discipline; at the second stage (1961–1990), intensive development of radioecology was noted, and at the third stage (1991–2010) — progressive development of radioecology; the forth modern stage of radioecology development falls at the beginning of the twentieth century (2011 — present). For each stage the main scientific achievements and evolution of ideas in the field of radioecology are considered. It is postulated that at present the development of this discipline is associated with the further improvement of world nuclear technologies, the elimination of the consequences of a number of radiation incidents (the accident at the Fukushima nuclear power plant, 2011), the revision of the concept of radiation protection of the environment and a number of other provisions. Particular attention is paid to forest radioecology, one of the most important main directions of this science.

We studied 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 region) in 2019, i.e. 6 years after local precipitation of ¹³⁷Cs due to a radiation incident. Morphological features of the upper horizons of urban soils were: brownish-gray color, light-loamy composition, small-lumpy and lumpy structure, inclusions of construction and household waste. In the upper horizons of urbiquasizems 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 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 is an increase in the specific activity of ²²⁶Ra. Some technogenic horizons 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 composition and properties of upper horizons formed as a result of excavation and decontamination work.