Non-eroding speed of water flow of channels running in cohesive soils

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.