Transformation of Carbon and Humus in Irrigated Meadow Soils of Deserts

dc.contributor.author	Askarov Khasanboy Kholdorovich
dc.date.accessioned	2025-12-29T18:27:58Z
dc.date.issued	2023-11-30
dc.description.abstract	Accumulation of soil carbonates in the soil profile occurs mainly during the evaporation of mineralized groundwater in the modern hydromorphic stage of soil formation, and not during soil formation. assortment of plant residues. The increase in organic carbon in irrigated soils is associated with an increase in the recency of development and cultivation.
dc.format	application/pdf
dc.identifier.uri	https://webofjournals.com/index.php/8/article/view/423
dc.identifier.uri	https://asianeducationindex.com/handle/123456789/25589
dc.language.iso	eng
dc.publisher	Web of Journals Publishing
dc.relation	https://webofjournals.com/index.php/8/article/view/423/403
dc.rights	https://creativecommons.org/licenses/by-nc-nd/4.0
dc.source	Web of Agriculture: Journal of Agriculture and Biological Sciences; Vol. 1 No. 8 (2023): WOA; 86-92
dc.source	2938-3781
dc.subject	pedogen, carbon, lithogen, humus, organic carbon, mineral carbon, conservative, soil cover, accumulation.
dc.title	Transformation of Carbon and Humus in Irrigated Meadow Soils of Deserts
dc.type	info:eu-repo/semantics/article
dc.type	info:eu-repo/semantics/publishedVersion
dc.type	Peer-reviewed Article

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