2021
DOI: 10.1088/1757-899x/1030/1/012121
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Results of a numerical study of currents in the vicinity of a damless water intake

Abstract: The problem of sustainable water intake in the conditions of significant fluctuations of flow rates and water level is significantly exacerbated by erosion of river beds. A typical example of such conditions is the damless water intake into the Karshi Main Canal (KMC) where the main flow of the Amudarya river continuously moves along a wide floodplain, changing the direction of currents. As a result, it is very difficult to withdraw the required volume of water from the river to the canal especially during dry… Show more

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Cited by 44 publications
(53 citation statements)
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“…From the point of view of vibration strength in units, the most dangerous are oscillations of a periodic nature, which are the result of mechanical, electromagnetic and hydraulic processes with pronounced discrete components. Such dangerous fluctuations are mainly strong diagnostic signals (that is, they stand out well against the background of vibration noise) [25][26][27].…”
Section:  mentioning
confidence: 99%
“…From the point of view of vibration strength in units, the most dangerous are oscillations of a periodic nature, which are the result of mechanical, electromagnetic and hydraulic processes with pronounced discrete components. Such dangerous fluctuations are mainly strong diagnostic signals (that is, they stand out well against the background of vibration noise) [25][26][27].…”
Section:  mentioning
confidence: 99%
“…To ensure a guaranteed volume of water with a minimum volume of bottom and suspended sediments is considered an urgent task. The dynamics of the hydraulic and alluvial flow regimes in the bed of the pumping station inlet channels were studied in [7][8][9][10][11][12][13][14][15]. Sediments occur due to the hydrodynamic effect of the flow on the stand plate in the presence of cavitation, eroding water flow rate in the channels, and dynamic instability of large soil channels with wind waves [16][17][18].…”
Section: Introductionmentioning
confidence: 99%
“…As already mentioned above, there has recently been a sharp change in the hydrological regime of the river. There are intense deformations of the supply channel border since it runs on easily washed-out soils [19][20][21][22][23][24][25][26][27][28][29].…”
Section: Introductionmentioning
confidence: 99%
“…Where: is horizontal drainage depth, m; Н is drainage rate or critical groundwater depth, m; Н is final (residual) head, m; ℎ о is water filling depth, m. The drainage rate is the minimum depth of groundwater at which there will be no salinization, and it depends on plants (cereals, alfalfa, and cotton), capillary, and waterphysical properties of the soil and climatic conditions [17][18][19][20][21][22][23][24][25][26].…”
Section: Introductionmentioning
confidence: 99%