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Soil polygenesis in the northeast part of Vladimir opolieстатья
Информация о цитировании статьи получена из
Web of Science
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 13 марта 2026 г.
- Авторы: Alifanov V.M., Gugalinskaya L.A., Ivannikova L.A., Ovchinnikov A.Yu
- Журнал: Eurasian Soil Science
- Том: 39
- Номер: S1
- Год издания: 2006
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: S31
- Последняя страница: S39
- DOI: 10.1134/s1064229306130072
- Аннотация: Soil studies in cultural landscapes of the medieval epoch within the Vladimir opolie territory on theRussian Plain suggest that virtually all automorphic soils in this area were plowed in that period. The morphology of the profiles of studied soils depends on the composition of parent materials. If the parent material represents a pedocyclith that passed through the stage of periglacial pedogenesis in the Late Pleistocene, then thesoil profile developed from this material is a heterochronous body with distinct features of polygenesis. If theparent material is a relatively homogeneous sediment that was not subjected to periglacial pedogenesis in theLate Pleistocene, then the soil profile developed from this material contains only the features of the Holocenepedogenesis, even in the case when the thickness of the homogeneous substrate does not exceed 0.5 m. It ishypothesized that the Holocene pedogenesis within the humid forest and southern taiga zones in the center ofthe Russian Plain cannot delete the features of the pre-Holocene pedogenesis and morpholithogenesis; thesefeatures are always inherited by the profiles of modern soils. The presence of these features ensures the development of a fully developed mature soil profile
- Добавил в систему: Овчинников Андрей Юрьевич