Mathematical modeling of the dynamics of sedimentation as a factor in eutrophication of the water masses of the Kuibyshev reservoir

In the study of the dynamics of the formation conditions of the underwater topography of large reservoirs along with the morphology of the basin and the nature of the collapse of the coast of great importance score hydrodynamic activity of water masses, which is associated with regulation of the flow regime. In this paper, based on model experiments investigated the spatial variability of sediment distribution and heterogeneity of phosphorus in Kuibyshev Reservoir the in the deep-water area near the dam.