kaz65Почвоведение и агрохимияSoil Science and Agrichemistry1999-740X2959-3433Казахский научно-исследовательский институт почвоведения и агрохимии имени У.У. Успановаkaz65-497Research ArticleГенезис и география почвSoil genesis and geographyГЕНЕЗИС, СВОЙСТВА И УЛУЧШЕНИЕ ПОДЗОЛИСТЫХ ЧЕРНОЗЕМОВ ЗАПАДНОЙ ЛЕСОСТЕПИ УКРАИНЫGENESIS, PROPERTIES AND AMENDMENT OF PODZOLISED CHERNOZEMS OF THE WEST FOREST-STEPPE IN UKRAINEМатвеевА.MatviivG. .annytas89@mail.ruКравченкоЮ.KravchenkoY. .kravch@i.uaНациональный университет биоресурсов и природопользования УкраиныУкраинаNational University of Life and Environmental Sciences of Ukraine; Soil Science and Soil Conservation DepartmentUkraine201607112022021016Copyright © Матвеев А..., Кравченко Ю..., 20222022Матвеев А., Кравченко Ю.Matviiv G..., Kravchenko Y...Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://journal.soil.kz/jour/article/view/497

В даннои обзорнои работе представлены подзолистые черноземы Украины. Черноземы как известно являются наиболее плодородными почвами, среди которых выделяются подтипы подзолистых черноземов согласно Украинскои классификации почв, сформированные преимущественно на возвышенностях лесостепи в западнои и восточнои части Украины. В статье описываются локальные черноземные факторы: климат, растительность, рельеф, почвообразующие породы, а также раионы их распространения. Проанализированы особенности генезиса, морфологические и другие своиства подзолистых черноземов в зависимости от местных условии и их использования. Описаны и обсуждены почвозащитные технологии, которые принимаются на подзолистых черноземах.

This review paper introduces the Podzolised chernozems in West Ukraine. Chernozems are reputed as the most productive and fertile soils of which Podzolised chernozem takes the position of the subtype in Ukrainian system of Soil Classification and covers minor highland of Forest-Steppe areas in the west and east of Ukraine. The paper describes the local Podzolised chernozem formation factors: general climate, vegetation, topography, parent materials and areas of their distribution. It has been reported particularities of genesis, morphology and other properties of Podzolised chernozem depending of local conditions and management. Soil conservation practices of Podzolised chernozems were also outlined and discussed in this paper.

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The authors declare that there are no conflicts of interest present.