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Please use this identifier to cite or link to this item: http://dspace.bsu.edu.ru/handle/123456789/59438
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dc.contributor.authorLisetskii, F. N.-
dc.contributor.authorBuryak, Zh. A.-
dc.contributor.authorMarinina, O. A.-
dc.contributor.authorUkrainskiy, P. A.-
dc.contributor.authorGoleusov, P. V.-
dc.date.accessioned2024-01-17T08:51:23Z-
dc.date.available2024-01-17T08:51:23Z-
dc.date.issued2023-
dc.identifier.citationFeatures of soil organic carbon transformations in the southern area of the East European Plain / F.N. Lisetskii, Buryak Zh.A., O.A. Marinina [et al.] // Geosciences. - 2023. - Vol.13, №9.-Art. 278. - URL: https://www.mdpi.com/2076-3263/13/9/278.ru
dc.identifier.urihttp://dspace.bsu.edu.ru/handle/123456789/59438-
dc.description.abstractThe active development of the problems related to the assessment of the role of the pedosphere in global climate change involves the possibility of application of the quantitative determination of soil organic carbon (SOC) as one of the indicators of a climatic response. Here, the authors have summarized the results of their own research over many years (1985-2023), comprising more than 500 determinations of SOC within the area of the Chernozem zone, in the south of the East European Plainru
dc.language.isoenru
dc.subjectsoil propertiesru
dc.subjectsoil organic carbonru
dc.subjectclimatic energy consumptionru
dc.subjectcarbon sequestrationru
dc.subjectcarbon poolsru
dc.subjectploughed landru
dc.subjectfallow landru
dc.titleFeatures of soil organic carbon transformations in the southern area of the East European Plainru
dc.typeArticleru
Appears in Collections:Статьи из периодических изданий и сборников (на иностранных языках) = Articles from periodicals and collections (in foreign languages)

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