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Study of evolution and fertility of degraded soils in the Kashkadarya river cone spread

Lazizakhon GafurovaNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanMirjalol KurbanovNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanSaidjon SidiqovNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanOlimaxon ErgashevaNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanZamira AbdushukurovaNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanSalomat ZakirovaNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanSayyorakhon YunusovaNational University of Uzbekistan named after Mirzo Ulugbek, 4 University Street, 100174 Tashkent, UzbekistanHafiza ArtiqovaBukhara State University, Uzbekistan, Bukhara, Uzbekistan
E3S Web of Conferencesjournal2024en
ABI

Аннотация

This article provides insights into the evolution of degraded soils in the Kashkadarya cone spread and the current factors influencing it. A comprehensive assessment of agrophysical, agrochemical, chemical, and microbiological properties of the degraded pale gray soils is presented, accompanied by the development of agricultural measures aimed at enhancing soil fertility. In the middle and lower segments of the cone, notable variations exist, as highlighted by M.A. Pankov. Flat elevations are characterized by light sandy and sandy soils, whereas the slopes of these elevations exhibit heavy and medium sandy soils. Flat depressions, on the other hand, feature clayey soils. This pattern extends to the bedrock within the soil, where the mechanical composition ranges from sand and loam to heavy sand and silt. In heavy sandy layers, there are occurrences of sand and silt layers and lenses, contributing to the overall mechanical composition.

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