TRANSFORMATION OF CLAY-MINERALS IN SOILS WITH THE TEXTURALLY-DIFFERENTIATED PROFILE

Authors
GOGOLEV AI DRONOVA TY SOKOLOVA TA TARGULIAN VO
Citation
Ai. Gogolev et al., TRANSFORMATION OF CLAY-MINERALS IN SOILS WITH THE TEXTURALLY-DIFFERENTIATED PROFILE, Eurasian soil science, 29(11), 1996, pp. 1274-1282
Citations number
24
Categorie Soggetti
Agriculture Soil Science
Journal title
Eurasian soil science → ACNP
ISSN journal
10642293
Volume
29
Issue
11
Year of publication
1996
Pages
1274 - 1282
Database
ISI
SICI code
1064-2293(1996)29:11<1274:TOCISW>2.0.ZU;2-I
Abstract
Three different types of texturally-differentiated soils (gley solod, podbel (Planosol), and pod-zolized red ferrallitic soil) are character ized by the development of the processes of clay peptization in the ho rizon A2B and lessivage. The destruction of clay minerals is more evid ently revealed in the acid soils (podbel and podzolized red ferralliti c). In the solod, soil material is enriched in illite throughout the w hole profile and clay minerals are very finely dispersed.