Results 1 to 10 of about 11,561 (252)
A Long‐Lived Planetesimal Dynamo Powered by Core Crystallization
The existence of numerous iron meteorite groups indicates that some planetesimals underwent melting that led to metal‐silicate segregation, sometimes producing metallic cores.
Clara Maurel +2 more
exaly +2 more sources
Effect of the Planetesimal Belt on the Dynamics of the Restricted Problem of 2 + 2 Bodies
In this paper, we study the existence and stability of collinear and noncollinear equilibrium points within the frame of the perturbed restricted problem of 2 + 2 bodies by a planetesimal belt.
Govind Mahato +2 more
exaly +3 more sources
Planetesimal formation starts at the snow line [PDF]
Planetesimal formation stage represents a major gap in our understanding of the planet formation process. The late-stage planet accretion models typically make arbitrary assumptions about planetesimals and pebbles distribution while the dust evolution ...
Joanna Drazkowska, Yann Alibert
exaly +4 more sources
Low strength and a shared size distribution connect the hot and cold Kuiper belt populations [PDF]
Understanding how the observed size distribution of Kuiper Belt objects emerged from the primordial planetesimal population remains a major challenge in planetary science.
P. G. Benavidez +3 more
doaj +2 more sources
Turbulence driven by magnetorotational instability (MRI) affects planetesimal formation by inducing diffusion and collisional fragmentation of dust particles.
Satoshi Okuzumi, Shigenobu Hirose
exaly +3 more sources
Recurrent planetesimal formation in an outer part of the early solar system [PDF]
The formation of planets in our solar system encompassed various stages of accretion of planetesimals that formed in the protoplanetary disk within the first few million years at different distances to the sun.
Wladimir Neumann +3 more
doaj +2 more sources
Size Ranges of Magnetic Domain States in Tetrataenite
Paleomagnetic studies of meteorites provide unique constraints on the evolution of magnetic fields in the early solar system. These studies rely on the identification of magnetic minerals that can retain stable magnetizations over ≳4.5 billion years (Ga).
Elias N. Mansbach +5 more
doaj +1 more source
We model the early stages of planet formation in the solar system, including continual planetesimal formation, and planetesimal and pebble accretion onto planetary embryos in an evolving disk driven by a disk wind.
John Chambers
doaj +1 more source
Planetesimal Initial Mass Functions Following Diffusion-regulated Gravitational Collapse
The initial mass function (IMF) of planetesimals is of key importance for understanding the initial stages of planet formation, yet theoretical predictions so far have been insufficient in explaining the variety of IMFs found in simulations.
Konstantin Gerbig, Rixin Li
doaj +1 more source
Ice Sublimation in Planetesimals Formed at the Outward Migrating Snowline
Isotopic studies of meteorites suggest that planetesimals were formed as two distinct populations: noncarbonaceous (NC) and carbonaceous (CC) reservoirs.
Zhongtian Zhang
doaj +1 more source

