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dc.contributor.author | Giniyatullin K. | |
dc.contributor.author | Shinkarev A. | |
dc.contributor.author | Krinari G. | |
dc.contributor.author | Lygina T. | |
dc.contributor.author | Gubaidullina A. | |
dc.contributor.author | Kornilova A. | |
dc.contributor.author | Mel'nikov L. | |
dc.date.accessioned | 2018-09-18T20:16:13Z | |
dc.date.available | 2018-09-18T20:16:13Z | |
dc.date.issued | 2012 | |
dc.identifier.issn | 1064-2293 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/138168 | |
dc.description.abstract | The relationship between the fixation of organic matter into a form resistant to oxidative destruction and the actual structure of the clay component was studied in profiles of different-aged chernozemic soils of a filled fortification in the Volga Bulgaria. With the use of modern methods (X-ray phase analysis, laser diffraction granulometry, hyphenated thermal analysis-FT-IR spectroscopy, adsorption-luminescence analysis, and ICP emission spectroscopy), it was shown that the formation of organic-smectite complexes with a disordered c*-axis structure is a universal and usual way for the kinetic stabilization of the system during pedogenesis under forest-steppe conditions. The main aim of the study was to experimentally substantiate this phenomenon. © 2012 Pleiades Publishing, Ltd. | |
dc.relation.ispartofseries | Eurasian Soil Science | |
dc.title | Irreversible fixation of organic components in labile interspaces as a mechanism for the chemical stabilization of clay-organic structures | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 11 | |
dc.relation.ispartofseries-volume | 45 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 1068 | |
dc.source.id | SCOPUS10642293-2012-45-11-SID84869047708 |