Derivation of the non-linear shallow water equations over unsaturated porous media: a discontinuous galerkin method for coarse-grained beaches
Résumé
This work will consider the physics of free-surface flow and groundwa-
ter flow in a coupled model. Coupled models of such phenomena are not
clearly justified, and there is a lack of precision in deriving such a model.
The primary aim of this work is to derive a coupled model of Shallow Wa-
ter Equations (SWE) and Richards’ Equation (RE) using asymptotic con-
siderations. The numerical coupling chosen for the unified model will be
explained as a parallel coupling. Additionally, numerical considerations on
how to solve this model using Discontinuous Galerkin (DG) methods will
be provided. Furthermore, explanations will be given about how informa-
tion is exchanged between the two models, which are time-synchronized.
The solution of RE coupled with SWE using the mentioned procedure
with DG formulation is implemented in RIVAGE (an in-house numerical
code based on discontinuous Galerkin method), which is then tested on a
numerical problem and validated against an experimental benchmark.
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