DOI:
https://doi.org/10.37547/tajas/Volume02Issue09-40Keywords:
Bank deformationAbstract
This article analyzes the factors influencing the occurrence of the deformation process in the channels based on the information obtained in the natural field conditions. The processes taking place in the Sokhsay river basin in the Sokh river basin were analyzed. During the research: The morphometry, flow rate and turbidity of the Sokhsay river were studied.
References
Arifjanov A.M., Fathulloev A.M. Dinamika vzvesenesushchego potoka v ruslah. [Dynamics of a suspended flow in the channels]. Fan. Tashkent, 2014. 124 p. (In Russian)
Arifjanov AM, Fatkhullaev AM, Samiev LN, Ozandagi Jarayonlar va daryo cho'kindilari. [Processes in Uzgen and river sediments]. Tashkent, 2017. Monograph. The light of the publisher, 191p. (In Uzbek)
Arifjanov A.M. Metody raschota raspredeleniya chastits nanosov v ruslakh peremennogo secheniya[Methods for calculating the distribution of particles of sediment in the channels of variable cross-section]. Hydrotechnical Construction. Moscow, 2004. No4. Pp.50-54. (In Russian)
Arifjanov А. Raspredeleniye vzveshennykh nanosov v statsionarnom [Distribution of suspended sediment in the stationary flow]. Water resources. Moscow, 2011. No2. Pp. 185-187. (In Russian)
Arifjanov A.M., Samiev L.N., Ahmedov I.G. Irrigatsionnoe zhnachenie rechnykh nanosov [The irrigational
