
The aggregation of dust grains into planetesimals in protoplanetary disks.Planetesimal formation is the process by which microscopic dust grains in a protoplanetary disk—a rotating disk of gas and dust around a young star—stick together and grow into kilometer-sized bodies called planetesimals. These are the building blocks of planets; once formed, they can collide and merge to create terrestrial planets, and their gravity can attract gas to form giant planets. The process bridges the gap between dust and planets, and it remains one of the most challenging steps in planet formation theory.
The concept dates back to the 1970s with Viktor Safronov's work on planet formation, but the specific problem of the meter barrier was identified in the 1980s. The streaming instability was proposed by Andrew Youdin and Jeremy Goodman in 2005, and it has since become the standard mechanism in numerical simulations.
Dust grains collide and stick via electrostatic forces, growing from sub-micron sizes to millimeter pebbles. However, at sizes around a meter, they face the 'meter barrier': they drift rapidly toward the star due to gas drag and are lost. The leading solution is the streaming instability, where the presence of many pebbles in a gas disk creates a feedback that concentrates them into dense clumps. These clumps then collapse gravitationally to form planetesimals directly, bypassing the slow growth through collisions. Turbulence in the disk can also create vortices that trap dust and accelerate the process.
Understanding planetesimal formation is crucial for interpreting observations of protoplanetary disks (e.g., with ALMA) and for explaining the diversity of exoplanet systems, including the formation of rocky planets like Earth.
The streaming instability can concentrate pebbles into clumps that are thousands of times denser than the surrounding disk, making them collapse into planetesimals in just a few orbital periods.





















