Experimental studies of sharply changing movements of a saturated turbidity flow
Ochiq kirish: yoʻq
Annotatsiya
In this paper, the results of experimental studies on the sharply changing movement of a turbulent flow with intense turbidity, specific to the rivers of Algeria, fed by rain, are presented. The results of experimental studies have established that with an increase in the turbidity of the flow to a certain value, an increase in the average velocity is observed; within a certain value of turbidity, the flow rate remains almost unchanged; with a further increase from this turbidity value, a decrease in the value of the average flow velocity is observed. It was established that when a suspended flow moved along channels, three stages of velocity were observed in the experiments: A stage of increasing flow velocity with increasing turbidity. This stage in experiments extends to a turbidity of 130 g/l; Stage B is a decrease in flow rate with an increase in turbidity of more than 230 g/l; Stage B is a decrease in flow rate with an increase in flow turbidity of more than 230 g/l. Experiments have obtained data on the movement of suspended flows with turbidity from 50 to 450 g/l. These data make it possible to develop calculated dependencies for the hydraulic characteristics of a sharply changing turbulent flow of suspended turbidity and use them to compare calculated dependencies.
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