Ringed versus Ringless Worlds: How Poynting-Robertson Drag Shapes Rings across the Solar System
arXiv:2510.25302 · doi:10.3847/2041-8213/ae194b
Abstract
Planetary rings are not only ubiquitous around the giant planets in the outer Solar System, but have also been discovered around several small distant bodies. In contrast, no rings have been observed around any inner Solar System objects. To constrain the dynamical origin of this ringed-versus-ringless dichotomy, we employ a numerically cross-checked analytical model of gigayear-scale Poynting-Robertson (PR) drag due to the solar flux acting on an isolated particle, expressed as a function of the host body's heliocentric distance \(\,a_{\mathrm{pla}}\) and the particle radius \(\,r_{\mathrm{par}}\). Here we show that, in the absence of additional perturbations, PR drag alone can explain the observed ring architecture of the Solar System: outer planets and Centaurs/TNOs are able to retain rings for the age of the Solar System, whereas any rings around the inner planets are removed on much shorter timescales. Because the PR-drag lifetime scales steeply with heliocentric distance \(\bigl(τ_{\mathrm{decay}}\propto a_{\mathrm{pla}}^{2} \,r_{\mathrm{par}}\bigr)\), we predict that forthcoming surveys will reveal an ever-growing population of ring-bearing bodies in the distant Solar System.
Accepted for publication in ApJL
References in corpus (11)
- A ring system detected around the Centaur (10199) Chariklo
- The size, shape, density and ring of the dwarf planet Haumea from a stellar occultation
- On the Impact Origin of Phobos and Deimos I: Thermodynamic and Physical Aspects
- Ring Formation around Giant Planets by Tidal Disruption of a Single Passing Large Kuiper Belt Object
- Obliquity evolution of extrasolar terrestrial planets
- The two rings of (50000) Quaoar
- Formation of Centaurs' rings through their partial tidal disruption during planetary encounters
- The rings of Neptune
- Implications for the collisional strength of Jupiter Trojans from the Eurybates family
- Constraints on the initial mass, age and lifetime of Saturn's rings from viscous evolutions that include pollution and transport due to micrometeoroid bombardment
- Giga-Year Dynamical Evolution of Particles Around Mars