Preview

Soil Science and Agrochemistry

Advanced search

FEATURES OF MINERALOGICAL COMPOSITION OF STAGNIC CHERNOZEMS

Abstract

On fragments of the pliocene planation surface of the northern part of Moldova there formed specific soils called stagnic chernozems. In comparison with zonal chernozems, stagnic chernozems are characterized by hidden lamination of rock-forming solid, high content of clay minerals (among them - smectite and illite). Quantitative ratio of the latter minerals disclose affinity with modern alluvial compact soils, as well as with compact chernozems. Stagnic chernozems are considered as polygenetic soils.

For citations:


Alexeyev V.E., Cherbar' V.V., Burghelya A.N., Varlamov E.B. FEATURES OF MINERALOGICAL COMPOSITION OF STAGNIC CHERNOZEMS. Soil Science and Agrochemistry. 2009;(1):47-58. (In Russ.)

Views: 151


Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.


ISSN 0130-8475 (Print)