Dispersion of species is an important research area in water resources and environmental engineering. In this context, species can refer to suspended sediment concentration, salinity, micro-organism number, or other water quality parameters. Herein species transport in shallow waters is predicted by a 4 × 4 hyperbolic matrix system of conservation laws formed by including an extra depth-averaged species equation to the two-dimensional shallow water equations, assuming that the flow is nearly horizontal, the pressure field is hydrostatic, and the species are well-mixed in the vertical. In such a system the species concentration is transported passively with the fluid velocity.
The resulting hyperbolic system is again numerically solved by a Godunov-type scheme, where the governing equations are discretised spatially using finite volumes on cell-centred collocated quadtree grids, with a slope-limited HLLC scheme used to model the inviscid flux terms. Second-order accuracy is achieved using a MUSCL-Hancock method. The resulting numerical model is applied to predict the advection of depth-averaged species due to wind-induced circulation in a shallow circular lake with a non-uniform bathymetry after validated against benchmark test cases.
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(a) (b) (c) Pure advection of species concentration in a uniform velocity field: (a) velocity field; (b) Contours; (c) adapted quadtree grid. |
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(c) (d) Pure diffusion of species concentration: (a) surface plot; (b) contours; (c) analytical and numerically predicted concentration profiles across a diagonal of the domain; (d) adapted quadtree grid. |
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(d) Advection-diffusion of species concentration: (a) velocity field; (b) comparison of concentration profiles obtained using different slope limiters with the exact solutions at t = 2.8 and 3.1 s; (c) surface plot and adapted quadtree grid at t = 2.8 s; (d) surface plot and adapted quadtree grid at t = 3.1s. |
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(d) (e) (f) Advection of species due to wind-driven circulation in a circular shallow lake: concentration contours at different output time. |