Single singular shock formation via Hugoniot asymptotics during transition to the ridged regime
Determine whether, in the hyperbolic system of three conservation laws for film height and the two depth-averaged particle volume fractions governing bidisperse particle-laden thin-film flow down an incline, the transition from the settled regime to the ridged regime corresponds to Hugoniot loci that approach one another asymptotically so as to produce a single singular shock, rather than the multiple-shock structure observed in the bidensity case; and characterize the parameter conditions under which this behavior occurs.
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In the monodisperse and bidensity case, this is due to the Hugoniot curves of the states approaching each other asymptotically in the far field instead of intersecting. We pose as an open problem that as the system transitions from the settled to the ridged regime, the Hugoniot curves of the states approach each other asymptotically in a way such that a single singular shock forms, as opposed to the multiple shock structure in the bidensity case.