KOLMATAJLANGAN TUPROQLARDA TEMIR ELEMENTINING LITOPEDOGEOKIMYOSI
Abstract
This article presents the lithopedogeochemical characteristics of iron in irrigated clogged
soils. The content of gross iron in irrigated, calmated soils formed on the banks and alluvial cones of the
Sokh and Isafairam rivers ranges from 2.31-3.65% and is in the range of the standard for world soils.
Keywords
Iron,, soil,, ion,How to Cite
References
Виноградов А.П. Геохимия редких и рассеянных химических элементов в почвах. - М.: 1957. -
с.
Зимина Н.И. и др. Характеристика вводно-физических и химических свойств некоторых почв
Центральной Ферганы: Сб.науч.тр. Союз НИХИ. вып.18. -Т.: 1970. с. 67-81
Сотиболдиева Г.Т. Фарғона вилояти кольматажланган тупроқларининг биогеокимёвий
хусусиятлари ва улардан фойдаланиш.: дисс. Автореф. б.ф.ф.д. (PhD)- Т.: 2018. 40-б.
Абдухакимова, Х. А. (2021). Шохимардонсой конус ёйилмаси сугориладиган тупрокларининг
геокимёси. Б.ф.ф.д. дисс. автореф. Фаргона, 42.
Юлдашев, Ғ., Сотиболдиева, Г. Т., & Абдухакимова, Х. Х. (2020). Biogeochemical properties of
calcium and strontium in gray soils. Scientific Bulletin of Namangan State University, 2(5), 61-67
License
Copyright (c) 2023 Sotiboldiyeva Go‘zalxon,, Abduxakimova Xusnidaxon
This work is licensed under a Creative Commons Attribution 4.0 International License.
The content published on the International Scientific and Current Research Conferences platform, including conference papers, abstracts, and presentations, is made available under an open-access model. Users are free to access, share, and distribute this content, provided that proper attribution is given to the original authors and the source.
