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Dive into the research topics where B. M. Kondratenok is active.

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Featured researches published by B. M. Kondratenok.


Eurasian Soil Science | 2008

Formation of polycyclic aromatic hydrocarbons in northern and middle taiga soils

D. N. Gabov; V. A. Beznosikov; B. M. Kondratenok; E. V. Yakovleva

An integrated study of the qualitative and quantitative composition of polycyclic aromatic hydrocarbons (PAHs) in the atmospheric precipitation-soil-lysimetric water system was performed using high performance liquid chromatography. It was shown that the accumulation of low-molecular PAHs (phenanthrene, anthracene, fluoranthene, pyrene, benz[a]anthracene, and chrysene) in soils is due to the transformation of organic matter and the regional transport and deposition of PAHs with atmospheric precipitation on the underlying surface. High-molecular polyarenes (benz[b]fluoranthene, benz[k]fluoranthene, benz[a]pyrene, dibenz[a,h]anthracene, benzo[ghi]perylene, and indeno[1,2,3-cd]pyrene) mainly result from the decomposition of soil organic matter.


Eurasian Soil Science | 2007

Assessment of background concentrations of heavy metals in soils of the northeastern part of European Russia

V. A. Beznosikov; E. D. Lodygin; B. M. Kondratenok

The assessment of background concentrations of heavy metals in soils of the southern regions of the Komi Republic has been performed. Within the accumulative landscapes, soils are enriched with virtually all the studied heavy metals in comparison with the eluvial landscapes. A database of the content of heavy metals has been developed using GIS technologies, and maps showing the distribution of heavy metals in soils of the southern part of the Komi Republic have been obtained.


Eurasian Soil Science | 2012

Bioaccumulation of polycyclic aromatic hydrocarbons in the soil-plant systems of the northern-taiga biocenoses

E. V. Yakovleva; V. A. Beznosikov; B. M. Kondratenok; D. N. Gabov

Regularities in the formation of the pool of priority polycyclic aromatic hydrocarbons (PAHs) in the soil-plant systems of the northern taiga forest biocenoses were revealed. In soils and plants, PAHs mainly consisted of 3- and 4-nuclear structures. The content of polyarenes in plants on technogenically contaminated areas exceeded the background values by 2–5 times. The maximum bioconsumption of polyarenes was observed for bilberry leaves and Siberian spruce sprouts 4–5 years old. The highest mass fraction of PAHs was found in Siberian spruce plants of a mixed spruce-birch forest of the northern taiga. It was revealed that bilberry plants are hyperaccumulators of light PAHs.


Eurasian Soil Science | 2010

Saturated hydrocarbons in the background and contaminated soils of the cisurals

D. N. Gabov; V. A. Beznosikov; B. M. Kondratenok; I. V. Gruzdev

A homologous series of n-alkanes (C20–C35) was identified in peaty-podzolic-gleyic soils. Structures with odd numbers of carbon atoms (C25–C35) were predominant in the soil organic matter. It was found that the major amount of both odd and even n-alkanes was accumulated in the peaty litter. In the mineral horizons, the mass fraction of the odd n-alkanes abruptly decreased to become comparable to that of the even n-alkanes in the soil-forming rock.


Eurasian Soil Science | 2014

Complexation of mercury(II) ions with humic acids in tundra soils

R. S. Vasilevich; V. A. Beznosikov; E. D. Lodygin; B. M. Kondratenok

The interaction mechanisms of mercury(II) ions with preparations of humic acids (HAs) isolated from organic horizons of surface-gleyed soils (Haplic Stagnosol (Gelic, Siltic)) of shrub tundra and hydromorphic peat gley soils (Histic Cryosol (Reductaquic, Siltic)) of moss-lichen tundra have been studied. The particular features of the interactions between the mercury(II) ions and the HAs are related to the molecular structure of the HAs, the mercury concentration range, and the environmental parameters. The fixation of mercury(II) ions into stable coordination compounds is most efficient in the pH range of 2.5–3.5. At the element concentrations below 0.50 μmol/dm3, the main complexing sites of HAs are their peripheral aminoacid functional groups. Pyrocatechol, salicylate, and phenolic groups from the nuclear moiety of molecules interact in the concentration range of 0.0005–0.50 mmol/dm3; the physical sorption of mercury hydroxo complexes by the surface of HAs is the main process occurring in the system.


Geochemistry International | 2010

Polycyclic aromatic hydrocarbons in the soils of technogenic landscapes

D. N. Gabov; V. A. Beznosikov; B. M. Kondratenok; E. V. Yakovleva

An integrated study of qualitative and quantitative composition of polycyclic aromatic hydrocarbons (PAH) in the atmospheric precipitation-soil-lysimetric water system of aerotechnogenic polluted landscapes was conducted using high-performance liquid chromatography in a gradient mode. Only low-molecular weight polyarenes (phenanthrene, anthracene, fluoranthene, pyrene, benz(a)anthracene, and chrysene) were found in the atmospheric precipitation and lysimetric waters. The growth of PAHs in soils is provided by the input of phenanthrene, fluoranthene, and pyrene with atmospheric precipitation. The absence of heavy PAHs (benzfluoranthenes, benz(a)pyrene, dibenz(a,h)anthracene, benz(ghi) perylene, and indeno[1,2,3-cd]pyrene) in the atmospheric precipitation and their identification in soil give grounds to state that their accumulation was caused mainly by transformation of organic matter during pedogenesis. The technogenic impact was estimated and criterion of the degree of soil pollution by PAH was proposed.


Eurasian Soil Science | 2016

Accumulation of polycyclic aromatic hydrocarbons in soils and plants of the tundra zone under the impact of coal-mining industry

E. V. Yakovleva; D. N. Gabov; V. A. Beznosikov; B. M. Kondratenok

Thirteen polycyclic aromatic hydrocarbon (PAH) compounds were identified in organic horizons of tundra surface-gleyed soils ( Histic Stagnosols (Gelistagnic) and plants. The total content of PAHs in contaminated soils exceeded the background values by three times. Concentrations of low-molecular weight hydrocarbons in soils at different distances from the coalmines were relatively stable. Concentrations of highmolecular weight hydrocarbons had a distinct maximum at a distance of about 0.5 km from the source of emission. The increased values of correlation coefficients were found between PAH concentrations in organic soil horizons, plants, and coal of the Vorkutinskaya mine. Mostly low-molecular weight structures predominated in the organic soil horizons and in the studied plant species. The maximum capacity for the biological accumulation of PAHs was displayed by Pleurozium schreberi and the minimum capacity was displayed by Vaccinium myrtillus. Mosses and lichens actively absorbed polyarenes from the surface; most of the PAHs were transported into the plants. This phenomenon was not observed for Vaccinium myrtillus Concentrations of PAHs on the surface and in plant tissues decreased with an increase in the distance from the mine. Distribution of polyarenes in plant organs was nonuniform. Insignificant excess of concentration of polyarenes was found in dead part of Pleurozium schreberi in comparison with its living part. The accumulation of polyarenes in the leaves of Vaccinium myrtillus was higher than that in its stems and roots.


Eurasian Soil Science | 2014

Polycyclic aromatic hydrocarbons in soils and lower-layer plants of the southern shrub tundra under technogenic conditions

E. V. Yakovleva; D. N. Gabov; V. A. Beznosikov; B. M. Kondratenok

In soils and plants of the southern shrub tundra, 15 polycyclic aromatic hydrocarbons (PAHs) have been detected by high-performance liquid chromatography. Polyarenes in emissions, soil organic horizons, and plants mainly include low-molecular-weight PAHs: naphthalene, fluorine, and pyrene. The contents of the total PAHs in soils and plants exceed the background levels by 3–5 times. The distribution of polyarenes among the organs of the studied plants is nonuniform and depends on the plant species and technogenic load on the area. The studied plants include both hyperaccumulators of polyarenes (Pleurozium schreberi) and indicators of PAHs in the soil (Polytrichum commune). Pleurozium schreberi is the most abundant species in the areas under study, and it accumulates the largest mass fraction of PAHs. The differences in the accumulation of PAHs by the plants of the tundra and taiga zones have been revealed.


Contemporary Problems of Ecology | 2011

Genotoxic effects in Tradescantia plant (clone 2) induced by benzo(a)pyrene

E. V. Yakovleva; V. A. Beznosikov; B. M. Kondratenok; A. A. Khomichenko

This work surveys the genetic toxicity of benzo(a)pyrene added to soil for Tradescantia plants (clone 02). Different adaptation levels of Tradescantia (clone 02) to soil pollution with benzo(a)pyrene have been estimated. Plant adaptation was not observed at the morphological level, but found for the physiological and genetic (with every adaptation stage) levels. The products of benzo(a)pyrene metabolism act as auxin on plants influencing the growth of root biomass and the cell size.


Eurasian Soil Science | 2015

Metrological assessment of the methods for measuring the contents of acids and ion metals responsible for the exchangeable acidity of soils

E. V. Vanchikova; E. V. Shamrikova; N. V. Bespyatykh; E. V. Kyz”yurova; B. M. Kondratenok

Metrological characteristics—precision, trueness, and accuracy—of the results of measurements of the exchangeable acidity and its components by the potentiometric titration method were studied on the basis of multiple analyses of the soil samples with the examination of statistical data for the outliers and their correspondence to the normal distribution. Measurement errors were estimated. The applied method was certified by the Metrological Center of the Uralian Branch of the Russian Academy of Sciences (certificate no. 88-17641-094-2013) and included in the Federal Information Fund on Assurance of Measurements (FR 1.31.2013.16382).

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V. A. Beznosikov

Russian Academy of Sciences

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D. N. Gabov

Russian Academy of Sciences

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E. V. Yakovleva

Russian Academy of Sciences

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E. D. Lodygin

Russian Academy of Sciences

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A. A. Khomichenko

Russian Academy of Sciences

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E. V. Kyz”yurova

Russian Academy of Sciences

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E. V. Shamrikova

Russian Academy of Sciences

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E. V. Vanchikova

Russian Academy of Sciences

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I. V. Gruzdev

Russian Academy of Sciences

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M. I. Vasilevich

Russian Academy of Sciences

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