Programs with programs to take water from the river without dams

In the arid areas of river itself, direction flow is characterized by changes depending on its hydrological regime. As a result these changes, can be branched into several streams and distributed differently in terms quantity. passes through lightly washed soils, have different depths, hydraulic elements morphometry vary at intensities. Changes resistance as such affect water permeability streams. It should noted that, form morphometry, roughness stream shoreline may same constant size depth. This could Karshi Main Amu Bukhara Mashina canals, which receive most dam-free from Amudarya to irrigated Republic Uzbekistan. catchment areas, rapid washing riverbeds, uneven distribution velocity, distance dam intake facility away main complicate operating conditions reduce amount required enter canal during growing season.