Abstract
Based on the tensor analysis of water-sediment two-phase flow, the basic model equations for clear water flow and sediment-laden flow are deduced in the general curve coordinates for natural water variable-density turbulent flow. Furthermore, corresponding boundary conditions are also presented in connection with the composition and movement of non-uniform bed material. The theoretical results are applied to the calculation of the float open caisson in the construction period and good results are obtained.
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Hongwei, F. The study on three-dimensional mathematical model of river bed erosion for water-sediment two-phase flow. Acta Mech Sinica 12, 85–91 (1996). https://doi.org/10.1007/BF02486765
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DOI: https://doi.org/10.1007/BF02486765