Non-eroding speed of water flow of channels running in cohesive soils
Sobir EshevKarshi branch of Tashkent Institute of Irrigation and Agricultural Mechanization Engineers, 180100, Karshi, UzbekistanShakhboz LatipovKarshi Engineering Economic Institute, 180100, Karshi, UzbekistanAzizali QurbonovKarshi branch of Tashkent Institute of Irrigation and Agricultural Mechanization Engineers, 180100, Karshi, UzbekistanJasur SagdiyevKarshi branch of Tashkent Institute of Irrigation and Agricultural Mechanization Engineers, 180100, Karshi, UzbekistanMustafo BerdievTashkent Institute of Irrigation and Agricultural Mechanization Engineers, 100000, Tashkent, UzbekistanNurbek MamatovKarshi Engineering Economic Institute, 180100, Karshi, Uzbekistan
ABI
Аннотация
Abstract The authors of the article, on the basis of laboratory experiments, describe the kinematic the structure of the erosion rates of the water flow in the conditions of non-cohesive soil lying in the peceidal canals. A methodology for conducting laboratory experiments and analysis of the results tov research. Dependencies are proposed for determining non-eroding water flow rates taking into account the occurrence of the slopes of the trapezoidal canal.
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Показатели — AkademScholar · Скоро