NEW MODEL OF A STRUCTURE OF A LONGITUDINAL-HOMOGENEOUS TURBULENT STREAM
Model of the simplest type of longitudinally homogeneous flows was repeatedly revised. The article describes the basic background which served as the reason for understanding the imperfections of proposals made by Prandtl, Karman and others and necessity of their refinement. On the basis of the proofs of theorems about a thin layer with negative turbulent viscosity existing inside these flows and the existence of an inflection point on the mean velocity diagram the model of the turbulent flow is revised and some new results are obtained.