Evolution of Coated Grains in Spiral Shocks of Self-Gravitating Protoplanetary Disks
M. Podolak, L. Mayer, and T. Quinn

TL;DR
This study examines how ice-coated grains in protoplanetary disks evolve as they pass through spiral shocks, revealing rapid opacity changes that influence disk cooling and potential fragmentation into sub-stellar objects.
Contribution
It introduces a detailed analysis of grain opacity evolution in spiral shocks using radiation-hydrodynamics simulations, highlighting effects on disk cooling and fragmentation.
Findings
Opacity drops faster than standard models predict.
Ice migration affects grain opacity and thermal properties.
Faster cooling may promote disk fragmentation.
Abstract
We investigate the evolution of grains composed of an ice shell surrounding an olivine core as they pass through a spiral shock in a protoplanetary disk. We use published three-dimensional radiation-hydrodynamics simulations of massive self-gravitating protoplanetary disks to extract the thermodynamics of spiral shocks in the region between 10 and 20 AU from the central star. As the density wave passes, it heats the grains, causing them to lose their ice shell and resulting in a lowering of the grain opacity. In addition, since grains of different sizes will have slightly different temperatures, there will be a migration of ice from the hotter grains to the cooler ones. The rate of migration depends on the temperature of the background gas, so a grain distribution that is effectively stable for low temperatures, can undergo an irreversible change in opacity if the gas is temporarily…
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