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Hydrological Alterations and Soil Microbial Responses Under Prolonged Irrigation and Salinity Stress

Shakhobiddin M. TurdimetovDepartment of Agro‐Soil Science and Land Reclamation Gulistan State University Gulistan UzbekistanMokhinur M. MusurmanovaDepartment of Agro‐Soil Science and Land Reclamation Gulistan State University Gulistan UzbekistanGulom JurayevDepartment of Agro‐Soil Science and Land Reclamation Gulistan State University Gulistan UzbekistanBerdiyor Ixtiyor Ogli OmonboyevDepartment of Agro‐Soil Science and Land Reclamation Gulistan State University Gulistan UzbekistanMohamed Fawzy RamadanDepartment of Clinical Nutrition, Faculty of Applied Medical Sciences Umm Al‐Qura University Makkah Saudi ArabiaMuhammad AliDepartment of Microbiology Quaid‐i‐Azam University Islamabad Islamabad PakistanShabeena MajeedUniversity of MianwaliMuhammad Rizwan KhanDepartment of Plant Sciences Quaid‐i‐Azam University Islamabad Islamabad PakistanTrobjon MakhkamovDepartment of Botany and Genetics National University of Uzbekistan Tashkent UzbekistanAdnan AminDepartment of Life Sciences Yeungnam University Gyeongsan Republic of Korea
2026en

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ABSTRACT The Mirzachol Oasis is one of the most important agroecological regions in Uzbekistan and has been subject to six decades of intensified irrigation, resulting in significant hydrological and soil changes. The impact on microbial communities below the surface is less well studied than its impact on the surface, but both affect soil health. This study addresses this gap by examining microbial communities, soil physicochemical parameters and historical irrigation data from 1960–2020 across six separate plots, including protected and irrigated plots. The results show that, due to organic matter accumulation and cultivation, extended irrigation increased microbial diversity and biogenicity in nonsaline soils (such as the U. Nasir and Yangi Hayot massifs). Nevertheless, secondary salinization disrupted nutrient cycling by suppressing functional microbial guilds, such as nitrifiers and cellulose‐degrading bacteria, in irrigated zones (e.g., the M. Uzoqov and Pakhtakor massifs). The salinization legacy reduces ecosystem stability, while older irrigated soils exhibit greater microbial resilience than recently irrigated or protected lands. Microbial activity was further influenced by seasonal variations, pH changes and groundwater fluctuations; salinity exacerbated reductions in fungal and actinomycete populations.

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