Collisional damping in debris discs: Only significant if collision velocities are low
arXiv:2411.13991 · doi:10.1051/0004-6361/202451080
Abstract
Context. Dusty debris discs around main sequence stars are observed to vary widely in terms of their vertical thickness. Their vertical structure may be affected by damping in inelastic collisions. Although kinetic models have often been used to study the collisional evolution of debris discs, these models have not yet been used to study the evolution of their vertical structure. Aims. We extend an existing implementation of a kinetic model of collisional evolution to include the evolution of orbital inclinations and we use this model to study the effects of collisional damping in pre-stirred discs. Methods. We evolved the number of particles of different masses, eccentricities, and inclinations using the kinetic model and used Monte Carlo simulations to calculate collision rates between particles in the disc. We considered all relevant collisional outcomes including fragmentation, cratering, and growth. Results. Collisional damping is inefficient if particles can be destroyed by projectiles that are of much lower mass. If that is the case, catastrophic disruptions shape the distributions of eccentricities and inclinations, and their average values evolve slowly and at the same rate for all particle sizes. Conclusions. The critical projectile-to-target mass ratio (Yc) and the collisional timescale jointly determine the level of collisional damping in debris discs. If Yc is much smaller than unity, a debris disc retains the inclination distribution that it is born with for much longer than the collisional timescale of the largest bodies in the disc. Such a disc should exhibit a vertical thickness that is independent of wavelength even in the absence of other physical processes. Collisional damping is efficient if Yc is of order unity or larger. For millimetre-sized dust grains and common material strength assumptions, this requires collision velocities of lower than ~40 m/s. Abridged
pre-print of article published in Astronomy & Astrophysics, DOI: https://doi.org/10.1051/0004-6361/202451080; output data DOI: https://doi.org/10.5281/zenodo.14196398
References in corpus (17)
- Transience of hot dust around sun-like stars
- Variations on Debris Disks: Icy Planet Formation at 30-150 AU for 1-3 Solar Mass Main Sequence Stars
- Collisional processes and size distribution in spatially extended debris discs
- Outer edges of debris discs: how sharp is sharp?
- Kuiper Belt-Like Hot and Cold Populations of Planetesimal Inclinations in the Pictoris Belt Revealed by ALMA
- The Mass of Stirring Bodies in the AU Mic Debris Disk Inferred from Resolved Vertical Structure
- ALMA observations of the narrow HR 4796A debris ring
- Near-infrared emission from sublimating dust in collisionally active debris disks
- From Pebbles and Planetesimals to Planets and Dust: the Protoplanetary Disk--Debris Disk Connection
- The vertical structure of debris disks and the impact of gas
- Dust size and spatial distributions in debris discs: predictions for exozodiacal dust dragged in from an exo-Kuiper belt
- ALMA Observations of the HD~110058 debris disk
- Deprojecting and constraining the vertical thickness of exoKuiper belts
- Collisional Particle Disks
- Stirred but not shaken: a multi-wavelength view of HD 16743's debris disc
- Rave: A non-parametric method for recovering the surface brightness and height profiles of edge-on debris disks
- Multiwavelength Vertical Structure in the AU Mic Debris Disk: Characterizing the Collisional Cascade