The Amount of Different Forms of Iron Contained in Soils Formed in Tertiary Reddish Deposits

dc.contributor.author	M.X.Khakimova
dc.contributor.author	S.Z. Bo’riyeva
dc.date.accessioned	2026-01-01T12:08:31Z
dc.date.issued	2022-03-19
dc.description.abstract	In this work, the amount of various forms of iron in soils formed on tertiary red-colored deposits is compared with typical serozems formed on lyossian deposits, by horizons and levels of erosion. It has been established that the gross, silicate and nocilicate forms of iron in the soil are determined as a percentage of the soil mass.
dc.format	application/pdf
dc.identifier.uri	https://zienjournals.com/index.php/tjm/article/view/1040
dc.identifier.uri	https://asianeducationindex.com/handle/123456789/62824
dc.language.iso	eng
dc.publisher	Zien Journals
dc.relation	https://zienjournals.com/index.php/tjm/article/view/1040/844
dc.rights	https://creativecommons.org/licenses/by-nc/4.0
dc.source	Texas Journal of Multidisciplinary Studies; Vol. 6 (2022): TJM; 157-162
dc.source	2770-0003
dc.subject	Soil
dc.subject	ferrum
dc.subject	silicate
dc.subject	nosilicate
dc.title	The Amount of Different Forms of Iron Contained in Soils Formed in Tertiary Reddish Deposits
dc.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/publishedVersion
dc.type	Peer-reviewed Article

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