Are Pebble Pile Planetesimals Doomed? [PDF]
In parabolic flight experiments we studied the wind induced erosion of granular beds composed of spherical glass beads at low gravity and low ambient pressure. Varying g-levels were set by centrifugal forces. Expanding existing parameter sets to a pressure range between $p=300-1200\,$Pa and to g-levels of $g=1.1-2.2\,\rm m\,s^{-2}$ erosion thresholds ...
Tunahan Demirci +6 more
openaire +5 more sources
Chondrule formation by collisions of planetesimals containing volatiles triggered by Jupiter’s formation [PDF]
Chondrules are spherical or subspherical particles of crystallized or partially crystallized liquid silicates that constitute large-volume fractions of most chondritic meteorites.
Sin-iti Sirono, Diego Turrini
doaj +2 more sources
Testing the Jeans, Toomre, and Bonnor–Ebert Concepts for Planetesimal Formation: 3D Streaming-instability Simulations of Diffusion-regulated Formation of Planetesimals [PDF]
We perform streaming-instability simulations at Hill density and beyond to demonstrate that planetesimal formation is not completed when pebble accumulations exceed the local Hill density.
Hubert Klahr, Andreas Schreiber
openalex +3 more sources
Formation of dust-rich planetesimals from sublimated pebbles inside of the snow line [PDF]
Content: For up to a few millions of years, pebbles must provide a quasi-steady inflow of solids from the outer parts of protoplanetary disks to their inner regions.
Guillot, Tristan, Ida, Shigeru
core +2 more sources
Formation of rocky super-earths from a narrow ring of planetesimals [PDF]
A planetary origin model that forms exoplanets from a narrow ring of silicate material at a stellocentric distance of 1 au is able to explain the physical properties of super-Earths and reproduce the ‘peas in a pod’ pattern of uniformity within planetary
K. Batygin, A. Morbidelli
semanticscholar +1 more source
Isotopic trichotomy of main belt asteroids from implantation of outer solar system planetesimals [PDF]
Recent analyses of samples from asteroid (162173) Ryugu returned by JAXA's Hayabusa2 mission suggest that Ryugu and CI chondrites formed in the same region of the protoplanetary disk, in a reservoir that was isolated from the source regions of other ...
D. Nesvorný +4 more
semanticscholar +1 more source
Nucleosynthetic Pt isotope anomalies and the Hf-W chronology of core formation in inner and outer solar system planetesimals [PDF]
The Hf-W chronology of iron meteorites provides crucial information on the timescales of accretion and differentiation of some of the oldest planetesimals of the Solar System.
F. Spitzer +3 more
semanticscholar +1 more source
The Streaming Instability Cannot Form Planetesimals from Millimeter-size Grains in Pressure Bumps [PDF]
We present evidence that it is unlikely that the streaming instability (SI) can form planetesimals from millimeter grains inside axisymmetric pressure bumps.
D. Carrera, J. Simon
semanticscholar +1 more source
Thermophysical evolution of planetesimals in the primordial disc [PDF]
The primordial disc of small icy planetesimals, once located at 15–$30\, \mathrm{au}$ from the Sun, was disrupted by giant planet migration in the early Solar system.
B. Davidsson
semanticscholar +1 more source
From Pebbles and Planetesimals to Planets and Dust: The Protoplanetary Disk–Debris Disk Connection [PDF]
The similar orbital distances and detection rates of debris disks and the prominent rings observed in protoplanetary disks suggest a potential connection between these structures. We explore this connection with new calculations that follow the evolution
J. Najita, S. Kenyon, B. Bromley
semanticscholar +1 more source

