Перейти к основному содержанию
AkademIndex

Продукты

Для разработчиков

AkademBaseскороОткрытый API экосистемы
Латиница
Русский
Статья

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.

Темы

Идентификаторы

Цитирования и источники

Показатели — AkademScholar · Скоро