GEOCHEMICAL FACTOR OF DESERTIFICATION (11-14)

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Дата публикации статьи в журнале: 2020/06/11
Название журнала: Восточно Европейский Научный Журнал, Выпуск: 57, Том: 2, Страницы в выпуске: 11-14
Автор: Alibekov L. A.
, Samarkand State University , Professor
Автор: Fozilov H.H., Boymurodova S.E.
, Samarkand State University , Master degree
Автор: Tashmurodov J.
, Samarkand State University , Student
Анотация: The article discusses the natural types of landscape salinization in Central Asia. There are two types of salt accumulation – continental and Delta. In this work, based on the well-known geographical scheme of academician B. B. Polynov, the processes of continental type salinization of landscapes are described in detail. Further, the mechanisms of salinization of the Delite landscapes of the Bukhara and Karakul oases are covered in more detail. The author connects the formation of Delta landscapes and their geochemical features with tectonic structures on the basis of actual materials.
Ключевые слова: Natural types of landscape salinization   continental   deltaic   geomorphological schemes   climate   aridity   migration of chemical elements   migration of chemical elements  
Данные для цитирования: Alibekov L. A. , Fozilov H.H., Boymurodova S.E., Tashmurodov J. . GEOCHEMICAL FACTOR OF DESERTIFICATION (11-14). Восточно Европейский Научный Журнал. Географические науки. 2020/06/11; 57(2):11-14.

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