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Paleocryolithopedogenesis and Evolution of Soddy-Podzolic Soils of the Taiga Zone in the Northeast of the East European Plainстатья
Информация о цитировании статьи получена из
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 15 февраля 2024 г.
- Авторы: Ovchinnikov A.Yu, Khudyakov O.I., Khokhlova O.S., Makshanov A.M.
- Журнал: Eurasian Soil Science
- Том: 56
- Номер: 12
- Год издания: 2023
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 1911
- Последняя страница: 1924
- DOI: 10.1134/S1064229323602172
- Аннотация: The results of soil-genetic studies conducted on sod-podzolic soils in the Gryazovetsky district of the Vologda region are presented. The modern soils of the study area are represented by sod-podzolic soils of different variations (Albic Retisols) formed on loamy paleocryogenically transformed soil-forming rocks. The concept of the role of paleocryolithogenic processes that determined the formation and evolution of modern sod-podzolic soils of the north-east of the East European Plain is proposed. The considered set of paleocryolithopedogenic processes in modern zonal sod-podzolic soils allowed us to reconstruct the conditions for the formation of soils located in the periglacial region of the Valdai glaciation. The results obtained have expanded the understanding of the influence of the processes of Late Pleistocene cryogenesis and lithogenesis on the evolution of modern sod-podzolic soils of the northeast of the East European Plain. The obtained data show the processes forming the soils under consideration and for the first time it is proposed to isolate paleocryolithogenic soil combinations in the structure of the soil cover as a result of the combined natural process – paleocryolithopedogenesis.
- Добавил в систему: Овчинников Андрей Юрьевич