OROL DENGIZI QURIGAN TUBIDAGI DEGRADATSIYGA UCHRAGAN QOLDIQ O‘TLOQI SHO‘RXOKLAR

The article highlights the agrochemical properties of residual meadow salt

marshes formed as a result of global climate change on a dried seabed. Based on the results of

soil analysis, it was found that the content of nutrients varies. In subsequent years, as a result

of increased natural and anthropogenic impact in the Aral Sea region associated with the

drying of the Aral Sea, deterioration of the ecological situation, the rise of mineralized

groundwater in some areas close to the surface, with the intensification of drought and

desertification processes.

As a result of increased salinization processes, rising salt dust caused by storms led to

deterioration of agricultural land reclamation and a significant decrease in the content of

humus and nutrients in soils.