Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

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Найдено документов в текущей БД: 4

    Microbial Indication of Soils Contaminated with Industrial Emissions
[Text] / N. D. Sorokin, E. N. Afanasova // Contemp. Probl. Ecol. - 2011. - Vol. 4, Is. 5. - P508-512, DOI 10.1134/S1995425511050092. - Cited References: 26. - The work was carried out with financial support of RAS Programme no. 23, Project 1.3 "Succession Changes in Biodiversity in Technogenic Deteriorated Ecosystems of Siberia." . - 5. - ISSN 1995-4255
РУБ Ecology

Аннотация: Changes in the composition of microbial complexes and their biochemical activity in soil in the vicinity of a strong source of HF emission have been studied. A sharp decrease of the biomass, the number of asporous bacteria and actinomycetes, and a smaller decrease of the number of microscopic fungi has been revealed, along with a decrease in the enzymatic and respiratory activity of contaminated soil with the relative increase in the fraction of sporiferous bacteria. On the basis of the response of introduced population of Bacillus subtilis to different doses of HF, NaF, Na(2)SO(3) microbiological norm-fixing for technogenic soil ecosystems has been carried out.

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Держатели документа:
[Sorokin, N. D.] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia
[Afanasova, E. N.] Siberian Fed Univ, Krasnoyarsk 660041, Russia

Доп.точки доступа:
Sorokin, N.D.; Afanasova, E.N.

    Microbiological diagnostics of the status of pyrogenically changed pine forests in the Lower Angara River basin
[Text] / A. V. Bogorodskaya, N. D. Sorokin // Eurasian Soil Sci. - 2006. - Vol. 39, Is. 10. - P1136-1143, DOI 10.1134/S1064229306100115. - Cited References: 21 . - 8. - ISSN 1064-2293
РУБ Soil Science

Аннотация: The structure and functions of the microbial complexes in the soils after surface fires of different intensity were studied. The fires of high and medium intensity were found to lead to a significant decrease in the number and functional activity of microorganisms participating in the nitrogen-carbon cycle. The degree of changes in the postfire status of the soil microbocenoses was revealed to be related to the joint action of pyrogenesis and the hydrothermal conditions at the moment of the fire rather than to the fire intensity. The favorable combination of the elevated soil moisture and soil heating stimulates the microbiological processes of organic matter mineralization, thus, improving the forest-growing conditions for the pine forests. The microbial biomass, basal respiration, and the microbial metabolic coefficient are shown to adequately reflect the postfire status of the microbial complexes.

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Держатели документа:
Russian Acad Sci, Sukachev Inst Forestry, Siberian Div, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Bogorodskaya, A.V.; Sorokin, N.D.

    The state of microbial complexes in soils of forest ecosystems after fires and defoliation of stands by gypsy moths
[Text] / A. V. Bogorodskaya, Y. N. Baranchikov, G. A. Ivanova // Eurasian Soil Sci. - 2009. - Vol. 42, Is. 3. - P310-317, DOI 10.1134/S1064229309030089. - Cited References: 37. - This work was supported by the Russian Foundation for Basic Research (project no. 07-04-00562). . - 8. - ISSN 1064-2293
РУБ Soil Science

Аннотация: The state of microbial cenoses in the soils of forest ecosystems damaged by fires of different strengths and gypsy moth outbreaks (Central Siberia) was assessed by the intensity of the basal respiration, the content of carbon of the microbial biomass, and the microbial metabolic quotient. The degree of the disturbance of the microbial cenoses in the soils under pine forests after fires was higher than that in the soils under the forests defoliated by gypsy moths. The greatest changes of the microbial complexes were recorded after the fires of high and medium intensity. In the litters, the content of the microbial biomass, the intensity of basal respiration, and the microbial metabolic quotient value were restored on the fifth year after the fires, whereas in the upper (0-10 cm) soil layer, these parameters still differed from those in the control variant, especially after the highly intense fires. After the weak fires, the ecophysiological state of the microbial complexes was restored within two-three years.

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Держатели документа:
[Bogorodskaya, A. V.
Baranchikov, Yu. N.
Ivanova, G. A.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forestry, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Bogorodskaya, A.V.; Baranchikov, Y.N.; Ivanova, G.A.; Russian Foundation for Basic Research [07-04-00562]

    Post fire organic matter biodegradation in permafrost soils: Case study after experimental heating of mineral horizons
/ O. V. Masyagina, I. V. Tokareva, A. S. Prokushkin // Sci. Total Environ. - 2016. - Vol. 573. - P1255-1264, DOI 10.1016/j.scitotenv.2016.04.195. - Cited References:52. - The reported study was partially supported by the Russian Science Foundation (14-24-00113). . - ISSN 0048-9697. - ISSN 1879-1026
РУБ Environmental Sciences

Аннотация: Periodical ground fires of high frequency in permafrost forest ecosystems of Siberia (Russian Federation) are essential factors determining quantitative and qualitative parameters of permafrost soil organic matter. Specific changes in physical and chemical parameters and microbial activity of permafrost soil mineral horizons of northern taiga larch stands were revealed after heating at high temperatures (150-500 degrees C) used for imitation of different burn intensities. Burning at 150-200 degrees C resulted in decreasing of soil pH, whilst heating at 300-500 degrees C caused increase of pH compare to unheated soils. Water-soluble organic carbon concentration in permafrost soils heated at 150-200 degrees C was much higher than that of unheated soils. All these changes determined soil microbial activity in heated soils. In particular, in soils heated at 300-500 degrees C there was momentary stimulating effect on substrate-induced respiration registered and on basal respiration values in soils burned at 150 degrees C and 300-400 degrees C. Four-month laboratory incubation of permafrost soils heated at different temperatures showed stimulation of microbial activity in first several days after inoculation due to high substrate availability after heating. Then soon after that soil microbial community started to be depleted on substrate because of decreasing water-soluble organic carbon, C and N content and it continued to the end of incubation. (C) 2016 Elsevier B.V. All rights reserved.

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Держатели документа:
VN Sukachev Inst Forest SB RAS, 50-28 Akad Gorodok, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Masyagina, O. V.; Tokareva, I. V.; Prokushkin, A. S.; Russian Science Foundation [14-24-00113]