BIOGEOCHEMICAL ASPECTS OF THE GENESIS OF SALINE MARSHY SOILS

dc.contributor.authorYuldashev Gulom
dc.contributor.authorKhakimjonova Nazokatkhon
dc.date.accessioned2025-12-29T18:28:17Z
dc.date.issued2025-02-22
dc.description.abstractThe marshy soils formed in Central Fergana have been studied along with other hydromorphic soils. The research investigates the role of suspended sediments in soils under the influence of irrigation waters and water accumulation, as well as the partial role of ancient lake-alluvial deposits in soil genesis.
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dc.identifier.urihttps://webofjournals.com/index.php/8/article/view/3370
dc.identifier.urihttps://asianeducationindex.com/handle/123456789/25766
dc.language.isoeng
dc.publisherWeb of Journals Publishing
dc.relationhttps://webofjournals.com/index.php/8/article/view/3370/3328
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/4.0
dc.sourceWeb of Agriculture: Journal of Agriculture and Biological Sciences; Vol. 3 No. 2 (2025): WOA; 36-41
dc.source2938-3781
dc.subjectMarshy, grassland, hydromorphic, oxidation, reduction, gleying, alluvial, peat, accumulation, regeneration.
dc.titleBIOGEOCHEMICAL ASPECTS OF THE GENESIS OF SALINE MARSHY SOILS
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typePeer-reviewed Article

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