“…Among the possible general extensions, let us mention the case of heterogeneous maximal density constraints ρ ≤ ρ * (t, x) (see for instance [24], [38], [60] or [7] for applications to traffic flows). Depending on the applications, other reference fluid systems can be preferred to the classical Navier-Stokes equations: non-linear shallow water or Boussinesq equations for wave-structure interactions (see [38], [9], [36]), gradient flow formulations in the modeling of crowds [50], porous media equations and Hele-Shaw free boundary problems for tissue growth modeling (see for instance [35], [61]), Bingham equations for complex geophysical flows [21], etc. For the clarity of the presentation, we shall stick in this paper to the two "toy" systems (1.1) and (1.4) which already raise important and difficult analysis problems.…”