Biological and Ecological Engineering | Article | Published 2020
To assess the salt mix within the Sangzor basin geosystem (Uzbekistan, Mirzachul) is identified and shown on the flow map (according to IN Stepanov), which is a natural elementary spatial-temporal structure of the earth's crust. The currents are separated by geometric variation of the isogypsum lines of the topographic maps. For the first time in the geosystem of the Sangzor basin, the boundary of the flow areas is separated by the area of formation, transit and accumulation of water, salt and fine sand. The map shows geochemically compatible divergent and convergent regions, increasing regions of easily soluble salts and decreasing regions receiving natural salts