dc.contributor.author |
Shinkarev A. |
|
dc.contributor.author |
Giniyatullin K. |
|
dc.contributor.author |
Krinari G. |
|
dc.contributor.author |
Gnevashev S. |
|
dc.date.accessioned |
2018-09-17T21:15:18Z |
|
dc.date.available |
2018-09-17T21:15:18Z |
|
dc.date.issued |
2003 |
|
dc.identifier.issn |
1064-2293 |
|
dc.identifier.uri |
https://dspace.kpfu.ru/xmlui/handle/net/134742 |
|
dc.description.abstract |
Humus substances and metastable secondary aluminosilicates are considered as a self-organizing system of the clay-metal-organic soil complex; the special role of illite-smectite minerals is emphasized. The functional system of clay-metal-organic soil complex is defined as a nonadditive integration of processes and structures sufficient for ensuring the kinetic stability of humus substances and secondary aluminosilicate neoformations in the space-time continuum of interactions between living organisms and soil-forming rocks. Copyright © 2003 by MAIK "Nauka/Interperiodica" (Russia). |
|
dc.relation.ispartofseries |
Eurasian Soil Science |
|
dc.title |
Systems approach to the study of clay-humus interactions in soils |
|
dc.type |
Article |
|
dc.relation.ispartofseries-issue |
4 |
|
dc.relation.ispartofseries-volume |
36 |
|
dc.collection |
Публикации сотрудников КФУ |
|
dc.relation.startpage |
430 |
|
dc.source.id |
SCOPUS10642293-2003-36-4-SID9144274440 |
|