Experience in preparing the rock foundation of the Dnestr hydroelectric station

1981 ◽  
Vol 15 (8) ◽  
pp. 459-461 ◽  
Author(s):  
A. E. Azarkovich ◽  
M. I. Shuifer ◽  
A. I. Tsvetkov ◽  
S. S. Gandzyuk ◽  
E. L. Budnikov



1999 ◽  
Vol 33 (5) ◽  
pp. 313-319
Author(s):  
V. I. Sil’nitskii ◽  
V. A. Ulyashinskii


1979 ◽  
Vol 13 (8) ◽  
pp. 807-812 ◽  
Author(s):  
Z. I. Solov'eva


2018 ◽  
pp. 36-39
Author(s):  
N Ikramov ◽  
T Majidov

The article brings up data on sediment diversity at watercourse bed and on their movement in the form of ridges. The ridge form movement of sediment leads to the reduction of reservoir volume and canal cross section area, which has an effect on their carrying capacity, filling of pump station forechambers and hydroelectric station pressure basins with sediment. The presence of sediment in flow leads to abrasive deterioration of pumps, water motors and pressure pipes and to other negative consequences. Research work tasks on the study of these effects have been examined with the purpose of preventing such negative consequences. On the basis of laboratory data diagrams and relationships were obtained for ridge length, height and movement velocity vs. sediment hydraulic and geometric sizes.



1967 ◽  
Vol 1 (8) ◽  
pp. 684-689
Author(s):  
M. I. Gal'perin


Author(s):  
Dilip Mathur ◽  
Eric S. McClellan ◽  
Susan A. Haney


1977 ◽  
Vol 11 (3) ◽  
pp. 232-236 ◽  
Author(s):  
B. S. Kasatkin ◽  
V. Ya. Martenson ◽  
V. V. Volkov ◽  
I. I. Sushchuk-Slyusarenko ◽  
F. E. Doroshenko ◽  
...  


1984 ◽  
Vol 18 (4) ◽  
pp. 166-170
Author(s):  
A. L. Rakhmanova ◽  
I. O. Rybak


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