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Multi‐lithology stratigraphic model under maximum erosion rate constraint

Non‐linear single lithology or multi‐lithology diffusion models have been widely used by sedimentologists and geomorphologists in the field of stratigraphic basin simulations to simulate the large scale depositional transport processes of sediments. Nevertheless, as noticed by many authors, erosion and sedimentation processes are non‐symmetric. Soil material must first be produced in situ by weathering processes prior to be transported by diffusion. This is usually taken into account through a prescribed maximum erosion rate of the sediments, but no mathematical description of the coupling with the diffusion model has been proposed so far. In this paper, we introduce a new mathematical formulation for the coupling of the weather limited erosion and the multi‐lithology diffusion models, which appears as a non‐standard free boundary problem for a new variable acting as a limitor of the fluxes.