Results 11 to 20 of about 3,499 (221)
Planetesimals are born fragile and are subject to destruction by wind erosion as they move through the gas of a protoplanetary disk. In microgravity experiments, we determined the shear stress necessary for erosion of a surface consisting of 1 mm dust pebbles down to 1 Pa ambient pressure. This is directly applicable to protoplanetary disks.
L. Schönau +7 more
openaire +4 more sources
We investigate the orbital evolution of planetesimals in the inner disk in the presence of nebula gas and a (proto-) cold Jupiter. By varying the mass, eccentricity, and semimajor axis of the planet, we study the dependence of the relative velocities of ...
Kangrou Guo, Eiichiro Kokubo
doaj +2 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
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
On the Early Thermal Processing of Planetesimals during and after the Giant Planet Instability
Born as ice-rich planetesimals, cometary nuclei were gravitationally scattered onto their current orbits in the Kuiper Belt and the Oort Cloud during the giant planets’ dynamical instability in the early stages of our solar system’s history.
Anastasios Gkotsinas +4 more
doaj +3 more sources
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
Four new PLanetesimals Around TYpical and Pre-main seqUence Stars (PLATYPUS) debris discs at 8.8mm [PDF]
Millimetre continuum observations of debris discs can provide insights into the physical and dynamical properties of the unseen planetesimals that these discs host.
Wilner, David J. +15 more
core +1 more source
Planetesimal Growth in Evolving Protoplanetary Disks: Constraints from the Pebble Supply
In the core accretion model, planetesimals grow by mutual collisions and engulfing millimeter-to-centimeter particles, i.e., pebbles. Pebble accretion can significantly increase the accretion efficiency and help explain the presence of planets on wide ...
Tong Fang +4 more
doaj +1 more source
Pore Network Modeling of Core Forming Melts in Planetesimals
Early in the history of the solar system, planetesimals were differentiated into metallic cores. In some planetesimals, this differentiation took place by percolation of the denser core forming liquid through a lighter solid silicate matrix. A key factor
Giulio F. D. Solferino +2 more
doaj +1 more source
High-resolution Study of Planetesimal Formation by Gravitational Collapse of Pebble Clouds
Planetary embryos are built through the collisional growth of 10–100 km-sized objects called planetesimals, a formerly large population of objects, of which asteroids, comets, and Kuiper Belt objects represent the leftovers from planet formation in our ...
Brooke Polak, Hubert Klahr
doaj +1 more source

