CHANGES IN WATER DISCHARGE, TURBIDITY OF THE STREAM AND THE FLOW OF SUSPENDED SEDIMENTS OF THE RIVER. AMUDARYA IN THE UPPER POOL OF THE TAKHIATASH HYDROELECTRIC COMPLEX IN CONDITIONS OF REGULATED FLOW
O. S. AknazarovKarakalpak Institute of Agriculture and Agrotechnologies Karakalpakstan, UzbekistanK. T. KalenderovaKarakalpak Institute of Agriculture and Agrotechnologies Karakalpakstan, Uzbekistan
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The article is devoted to the study of changes in water flow, flow turbidity and runoff of suspended sediments of the Amudarya River in the upstream of the Takhiatash hydroelectric complex under conditions of regulated flow. For the analysis, long-term data of the Nietbaytas hydrological station, which is located in the zone of influence of the backwater of the Takhiatash shield dam, were used. As a result of the analysis, the features of the change in the regimes of liquid and solid runoff of the Amudarya River in the upper pool of the Takhiatash hydroelectric complex under conditions of regulated flow were revealed.
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