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 |
|