Skip to main navigation menu Skip to main content Skip to site footer

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

Abstract

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.

Keywords

Takhiatash hydroelectric complex, headwater, water

PDF

References

  1. Караушев А.В. Теория и методы расчета речных наносов. Л., Гидрометеоиздат, 1977, -288 с.
  2. Цветкова Н.А. Режим наносов р.Амударьи. //Вопросы гидротехники, в.13, Ташкент, 1963, с.5-86.
  3. Шульц В.Л. Реки Средней Азии. Л., Гидрометеоиздат, 1965, -692 с.
  4. Акназаров О.С. Совершенствование режима эксплуатации Тахиаташского гидроузла. Нукус, изд. «Илим», 2022, -133 с.