SO‘X KONUS YOYILMASI TUPROQLARINING AGROEKOLOGIK TAVSIFI

The head stone-gravel part of the river fan. Sokh is covered with calcified soils created artificially by man. In the middle and lower parts of the range, differing in the depth of the level and the mineralization of groundwater of the Saz regime, meadow-swamp-oasis and meadow-oasis soils are developed. The morphogenetic section of the soil, which is the result of hydromorphism processes, is composed of heterogeneous layers. In the middle part of the cone, the degree of soil salinity is weak, and to the north and the flanks of its periphery it increases. In terms of the amount of available phosphorus and potassium, soils belong to the groups of moderate and poor supply.