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. During landslides, the bulk of the sediment material (usually considered as a porous medium), transits from solid-like to fluid-like, i.e., from stagnant to continuously flowing. In addition, the coupling
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-fluid systems, with the help of Bayesian learning. Objectives: i) Understand the capabilities of fluid-solid models for granular media and their limitations to model the collapse of saturated granular
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charged polyelectrolytes at the interface of a porous support membrane. In this so-called Layer-by-Layer assembly, a support membrane is alternatively exposed to polycations and polyanions, to build
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