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Mineralization of Organic Matter in the Oil-Polluted and Background Soils of the Middle Ob Region under Laboratory Conditions

  • DEGRADATION, REHABILITATION, AND CONSERVATION OF SOILS
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Abstract—

In a laboratory experiment, the rate of mineralization of organic matter in samples of oil-contaminated and background soils formed in the main types of the middle-taiga biogeocenoses of Western Siberia was determined. The rate of mineralization was estimated by the amount of CO2 released from wet samples at room temperature. The cumulative curves had a linear form. Therefore, the values of the average daily CO2 release per 1 g of dry soil (Km) were used to estimate the mineralization rate. The Km values varied in the range of 0.1123–1.578 mg CO2/g per day. Minimum Km values (<0.2) were typical of the oil-polluted forest soils with the maximum content of oil products; high Km values (>0.8) were determined on the soils of uncontaminated background plots and oil-polluted plots of mesotrophic and eutrophic biogeocenoses with the neutral reaction and increased concentrations of biophilous elements. Moderate values (0.2 < Km <0.8) were typical of the plots confined to initially oligotrophic bogs (ryams, ridged-hollow bog complexes) moderately polluted with oil. The Km values negatively correlated with the contents of petroleum products (K = –0.50), n-alkanes (K = –0.73), and the coefficient of oil biodegradation (K = –0.72).

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Funding

The work was carried out within the framework of the state assignment with the Ministry of Science and Higher Education of the Russian Federation no. 121041300098-7 and no. 121040800147-0 and partly supported by the Development Program of the Interdisciplinary Scientific and Educational School of M.V. Lomonosov Moscow State University “The future of the planet and global environmental changes.”

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Correspondence to N. A. Avetov.

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Translated by D. Konyushkov

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Trofimov, S.Y., Arzamazova, A.V., Kinzhaev, R.R. et al. Mineralization of Organic Matter in the Oil-Polluted and Background Soils of the Middle Ob Region under Laboratory Conditions. Eurasian Soil Sc. 55, 533–540 (2022). https://doi.org/10.1134/S1064229322040147

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