Global Models of Runaway Accretion in White Dwarf Debris Disks
Brian D. Metzger, Roman R. Rafikov, Konstantin V. Bochkarev

TL;DR
This paper models the coupled evolution of gas and solids in white dwarf debris disks, revealing conditions under which runaway accretion occurs, explaining high metal accretion rates observed in some systems.
Contribution
It introduces a global time-dependent model of WD debris disks showing how gas-solid interactions can lead to runaway accretion, a novel mechanism for high metal accretion rates.
Findings
Runaway accretion can occur when gas builds up near sublimation radius.
The model's predicted accretion rates align with observed distributions.
Stronger solid-gas coupling increases likelihood of runaway accretion.
Abstract
A growing sample of white dwarfs (WDs) with metal-enriched atmospheres are accompanied by excess infrared emission, indicating that they are encircled by a compact dusty disk of solid debris. Such `WD debris disks' are thought to originate from the tidal disruption of asteroids or other minor bodies, but the precise mechanism(s) responsible for transporting matter to the WD surface remains unclear, especially in those systems with the highest inferred metal accretion rates dM_Z/dt ~ 1e8-1e10 g/s. Here we present global time-dependent calculations of the coupled evolution of the gaseous and solid components of WD debris disks. Solids transported inwards (initially due to PR drag) sublimate at tens of WD radii, producing a source of gas that accretes onto the WD surface and viscously spreads outwards in radius, where it overlaps with the solid disk. If the aerodynamic coupling between the…
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