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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 |