Viscously Stirring Particle Disks into Lorentzians and Gaussians to Infer Dynamical and Collisional Masses (ARKS XIII)
Eugene Chiang, Tim D. Pearce, Marija R. Jankovic, Alexander Jeffrey Backues, Yinuo Han + 14 more
TLDR
This paper explains how viscous stirring evolves particle disk vertical profiles from Lorentzian to Gaussian, inferring perturber masses.
Key contributions
- Viscous stirring causes a log-normal inclination distribution, leading to observed Lorentzian disk profiles.
- After sufficient scattering, inclinations equilibrate with eccentricities, relaxing profiles to Gaussian.
- Establishes an evolutionary sequence for particle disk vertical profiles from Lorentzian to Gaussian.
- Infers perturber masses (Moon-Earth or Pluto-sized) based on observed Lorentzian/Gaussian profiles.
Why it matters
This paper reconciles observed Lorentzian disk profiles with theoretical Gaussian assumptions by providing an evolutionary framework. It offers a physical mechanism for how particle disks evolve and allows for inferring the masses and collisionality of unseen stirring bodies, crucial for understanding planet formation.
Original Abstract
Disks (Keplerian or otherwise, particulate or fluid) are often assumed to have densities that drop off vertically as Gaussians. Recent mm-wave imaging of circumstellar debris disks contradicts this assumption, revealing vertical profiles in dust that resemble Lorentzians. As part of the ARKS ALMA Large Program, we calculate how Lorentzians and Gaussians define an evolutionary sequence for disks of gravitationally scattering (viscously stirring) particles. When orbits are crossing and eccentricities $e \gg$ inclinations $i$, each scattering changes a particle's inclination by $\pm \,Δi \propto i$. A random walk with fixed steps in $Δi/i = Δ\ln i$ produces a log normal $i$ distribution, whose thick tail at large $i$ leads to thick Lorentzian tails in density. This result holds independent of the origin of the large eccentricities; what matters is that relative motions parallel to the disk midplane are faster than perpendicular motions. After enough scatterings, $i$ comes into equipartition with $e$, $Δi$ stops exponentiating, and the vertical density profile relaxes to a Gaussian. We estimate the numbers and masses of perturbers needed to stir themselves and observable dust grains in Lorentzian and Gaussian debris disks imaged by ARKS. The big bodies may be sufficiently few in number as to be collisionless, in which case their masses range from the Moon to several Earths. But if Pluto-sized or smaller, the big body stirrers may be so numerous and collide so frequently that they can source the collisional cascades that produce observable dust.
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