Origin of compact exoplanetary systems during disk infall
arXiv:2505.22806 · doi:10.1038/s41467-025-60017-8
Abstract
Exoplanetary systems that contain multiple planets on short-period orbits appear to be prevalent in the current observed exoplanetary population, yet the processes that give rise to such configurations remain poorly understood. A common prior assumption is that planetary accretion commences after the infall of gas and solids to the circumstellar disk ended. However, observational evidence indicates that accretion may begin earlier. We propose that compact systems are surviving remnants of planet accretion that occurred during the final phases of infall. In regions of the disk experiencing ongoing infall, the planetary mass is set by the balance between accretion of infalling solids and the increasingly rapid inward migration driven by the surrounding gas as the planet grows. This balance selects for similarly-sized planets whose mass is a function of infall and disk conditions. We show that infall-produced planets can survive until the gas disk disperses and migration ends, and that across a broad range of conditions, the mass of surviving systems is regulated to a few 10^{-5} to 10^{-4} times the host star's mass. This provides an explanation for the similar mass ratios of known compact systems.
References in corpus (24)
- Gas- and dust evolution in protoplanetary disks
- The VLA/ALMA Nascent Disk and Multiplicity (VANDAM) Survey of Orion Protostars. A Statistical Characterization of Class 0 and I Protostellar Disks
- Density, not radius, separates rocky and water-rich small planets orbiting M dwarf stars
- Halting Type I planet migration in non-isothermal disks
- Formation of planetary systems by pebble accretion and migration: How the radial pebble flux determines a terrestrial-planet or super-Earth growth mode
- Close-in planetesimal formation by pile-up of drifting pebbles
- Dust masses of young disks: constraining the initial solid reservoir for planet formation
- Contacts of Water Ice in Protoplanetary Disks - Laboratory Experiments
- Hot super-Earths and giant planet cores from different migration histories
- Contemporary formation of early solar system planetesimals at two distinct radial locations
- Grain growth in the envelopes and disks of Class I protostars
- Magnetically self-regulated formation of early protoplanetary discs
- Planetesimal rings as the cause of the Solar System's planetary architecture
- Formation of Giant Planet Satellites
- Outflows, infall and evolution of a sample of embedded low-mass protostars. The William Herschel Line Legacy (WILL) survey
- A case of simultaneous star and planet formation
- Magnetospheric Gap and Accumulation of Giant Planets Close to the Star
- Are protoplanetary disks born with vortices? -- Rossby wave instability driven by protostellar infall
- Pushing planets into an inner cavity by a resonant chain
- Drifting inwards in protoplanetary discs II: The effect of water on sticking properties at increasing temperatures
- The influence of infall on the properties of protoplanetary discs
- Close-in Super-Earths: The first and the last stages of planet formation in an MRI-accreting disc
- Massive Protostellar Disks as a Hot Laboratory of Silicate Grain Evolution
- Planet formation and disk mass dependence in a pebble-driven scenario for low mass stars