Titlebook: Computational Hydraulics; An Introduction Cornelis B. Vreugdenhil Textbook 1989 Springer-Verlag Berlin Heidelberg 1989 Software.algorithm.c

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https://doi.org/10.1007/978-3-319-18138-7 this book. There are, however, certain situations in which they can be considerably simplified. Consider a quantity called the vorticity ., which is a measure of the rotation of a fluid particle about its axis (normal to the plane of flow; in 3-d the vorticity is a vector).

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https://doi.org/10.1007/978-3-319-18138-7e for suspended sand is . in which the sediment flux in vertical direction is . where . and . are the horizontal and vertical coordinates, . is the turbulent diffusion coefficient and . the settling velocity or fall velocity of the sand particles.