Explaining the variability of WD 1145+017 with simulations of asteroid tidal disruption
Dimitri Veras, Philip J. Carter, Zoe M. Leinhardt, Boris T. Gaensicke

TL;DR
This study uses numerical simulations to understand how asteroid properties influence their disintegration around white dwarf WD 1145+017, revealing that density and orbit eccentricity are key factors in their disruption timescale.
Contribution
It provides the first detailed numerical modeling of asteroid disintegration around WD 1145+017, linking physical properties to observed variability.
Findings
Disruption timescale depends strongly on density and eccentricity.
Differentiated rocky bodies can shed mass while remaining intact.
The orbiting asteroid is likely differentiated with a density similar to Vesta.
Abstract
Post-main-sequence planetary science has been galvanised by the striking variability, depth and shape of the photometric transit curves due to objects orbiting white dwarf WD 1145+017, a star which also hosts a dusty debris disc and circumstellar gas, and displays strong metal atmospheric pollution. However, the physical properties of the likely asteroid which is discharging disintegrating fragments remain largely unconstrained from the observations. This process has not yet been modelled numerically. Here, we use the N-body code PKDGRAV to compute dissipation properties for asteroids of different spins, densities, masses, and eccentricities. We simulate both homogeneous and differentiated asteroids, for up to two years, and find that the disruption timescale is strongly dependent on density and eccentricity, but weakly dependent on mass and spin. We find that primarily rocky…
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