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Acceptable water flow rate in sandy channels

Shakhboz LatipovKarshi engineering-economics institute, 180100 Karshi, UzbekistanJasur SagdiyevKarshi branch of Tashkent Institute of Irrigation and Agricultural Mechanization Engineers, 180119 Karshi, UzbekistanSobir EshevKarshi engineering-economics institute, 180100 Karshi, UzbekistanIslom KholmamatovKarshi engineering-economics institute, 180100 Karshi, Uzbekistanand Iroda RayimovaTashkent Institute of Irrigation and Agricultural Mechanization Engineers, 100000 Tashkent, Uzbekistan
E3S Web of Conferencesjournal2021en
ABI

Abstract

A comparison of the values obtained with the experimental data on noneroding velocity in the article shows that the soil erosion in the experiments took place much earlier because our experiments were carried out in trapezoidal channels, based on experiments in wide rectangular channels.

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