2016/04/14 by Shigeru Ida, S. Ida, Tristan Guillot +3 · 11 citations
Physics and Astronomy · #Accretion (finance) #Accretion disc #Astro and Planetary Science #Astrophysics and Star Formation Studies #Pebble #Planet #Planetary system #Planetesimal #Protoplanet #Solar System #Stellar, planetary, and galactic studies #astro-ph.EP
paper · pdf · doi:10.1051/0004-6361/201628099
published as A&A 591, A72 (2016) · 12 pages, 3 figures, accepted for publication in Astronomy & Astrophysics
arxiv created 2016/04/14 · openalex publication_date 2016/04/18 · arxiv updated 2016/06/22 · openalex created_date 2016/06/24 · openalex updated_date 2026/08/05
Context. The classical planetesimal accretion scenario for the formation of planets has recently evolved with the idea that pebbles, centimeter- to meter-sized icy grains migrating in protoplanetary disks, can control planetesimal and/or planetary growth.