The article investigates the morphogenetic characteristics and soil profile formation patterns of irrigated meadow alluvial soils. According to the study results, these soils are formed on alluvial deposits accumulated in river valleys, with their profile comprising humus, transitional, and illuvial horizons. Morphological analysis indicated that the humus horizon is characterized by a high content of organic matter and plant roots, while the lower horizons exhibit increased moisture, changes in mechanical composition, and the presence of iron and carbonate spots. Additionally, under irrigated agricultural conditions, anthropogenic factors were found to moderately alter the physical and chemical properties of the soil. The obtained results provide a scientific description of the genesis, morphological features, and morphogenetic characteristics of irrigated meadow alluvial soils.