Thermal hysteresis and front propagation in dense planetary rings
R\'emy Larue, Henrik Latter, Hanno Rein

TL;DR
This study uses N-body simulations with non-monotonic restitution laws to explore how dense planetary rings can exhibit multiple stable states and propagating fronts, shedding light on their complex structures.
Contribution
It introduces a novel simulation approach with non-monotonic restitution laws to model ring particle collisions, revealing multiple stable states and front propagation in planetary rings.
Findings
Existence of two thermally stable steady states at the same optical depth.
Warm states can migrate into colder states via traveling fronts.
Stationary viscous fronts connect states of different optical depth.
Abstract
Saturn's rings are composed of icy grains, most in the mm to m size ranges, undergoing several collisions per orbit. Their collective behaviour generates a remarkable array of structure over many orders of magnitude, much of it not well understood. On the other hand, the collisional properties and parameters of individual ring particles are poorly constrained; usually N-body simulations and kinetic theory employ hard-sphere models with a coefficient of restitution that is constant or a decreasing function of impact speed. Due to plastic deformation of surface regolith, however, it is likely that will be more complicated, at the very least a non-monotonic function. We undertake N-body simulations with the REBOUND code with non-monotonic laws to approximate surfaces that are friable but not sticking. Our simulations reveal that such ring models can support…
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