Abstract
This study examines the chemical composition and geochemical behavior of water-soluble salts in irrigated meadow saz soils, focusing on the impact of cemented shokh-arzyk horizons on salt migration and accumulation. Physicochemical analysis of soil samples from different genetic horizons revealed that the cemented layer significantly affects ion mobility, leading to variations in salt distribution.
The findings highlight the role of shokh-arzyk horizons in soil salinity dynamics and provide insights for improving soil fertility management in saline-affected regions.

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