Bouncing Grains Keep Protoplanetary Disks Bright
Yansong Qian, Yanqin Wu
TL;DR
This work addresses how protoplanetary disks remain millimeter-bright for several Myr, despite grain growth and radial drift. It argues that a bouncing barrier, capping grain growth at around $a_{\rm bounce} \approx 100\,\mu$m, suppresses drift and preserves optical thickness, thereby sustaining the observed size-luminosity relation and low spectral indices across regions from Lupus to Upper Scorpius. The authors combine multi-region disk data (including new USco measurements) with order-of-magnitude analytical estimates and DustPy simulations to contrast bouncing versus no-bouncing scenarios, finding that only bouncing can reproduce the long-lived, bright, compact disks. They also review observational evidence for small grains (e.g., mm polarization) and discuss theoretical caveats and the possible fate of disks after bounce, including how planetesimals might form without large grains. Overall, the bouncing barrier emerges as a robust, universal mechanism linking grain physics to disk observables and evolution, with implications for planetesimal formation and disk longevity.
Abstract
Proto-planetary disks display the so-called size-luminosity relation, where their mm-wavelength fluxes scale linearly with their emitting areas. This suggests that these disks are optically thick in mm-band, an interpretation further supported by their near-black-body spectral indexes. Such characteristics are seen not only among disks in very young star-forming regions like Lupus (1-3 Myrs), but, as we demonstrate here, also among disks in the much older Upper Scorpius region (5-11 Myrs). How can disks shine brightly for so long, when grain growth and subsequent radial drift should have quickly depleted their solid reservoir? Here, we suggest that the "bouncing barrier" provides the answer. Even colliding at very low speeds (below 1cm/s), grains already fail to stick to each other but instead bounce off in-elastically. This barrier stalls grain growth at a near-universal size of 100 micron. These small grains experience much reduced radial drift, and so are able to keep the disks bright for millions of years. They are also tightly coupled to gas, offering poor prospects for processes like streaming instability or pebble accretion. We speculate briefly on how planetesimals can arise in such a bath of 100-micron grains.
