Results 31 to 40 of about 2,944 (214)
Planetesimals in Debris Disks [PDF]
Planetesimals form in gas-rich protoplanetary disks around young stars. However, protoplanetary disks fade in about 10 Myr. The planetesimals (and also many of the planets) left behind are too dim to study directly. Fortunately, collisions between planetesimals produce dusty debris disks.
George H. Rieke, Andrew N. Youdin
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Erosion and the limits to planetesimal growth [PDF]
16 pages, 14 figures, accepted for publication in A& ...
Chris W. Ormel+4 more
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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
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Planetesimal and gas dynamics in binaries [PDF]
18 pages, 13 figures, accepted for publication in ...
Paardekooper, Sijme-Jan+2 more
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PLANETESIMAL COMPOSITIONS IN EXOPLANET SYSTEMS [PDF]
We have used recent surveys of the composition of exoplanet host stars to investigate the expected composition of condensed material in planetesimals formed beyond the snow line in the circumstellar nebulae of these systems. Of the major solid forming elements, we find that, as for the Sun, the C and O abundances (and particularly the C/O abundance ...
Olivier Mousis+4 more
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AF Lep A+b is a remarkable planetary system hosting a gas-giant planet that has the lowest dynamical mass among directly imaged exoplanets. We present an in-depth analysis of the atmospheric composition of the star and planet to probe the planet’s ...
Zhoujian Zhang+12 more
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Planetesimal Disk Evolution Driven by Planetesimal-Planetesimal Gravitational Scattering
29 pages, 1 figure, submitted to ...
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An Analytical Theory for the Growth from Planetesimals to Planets by Polydisperse Pebble Accretion
Pebble accretion is recognized as a significant accelerator of planet formation. Yet only formulae for single-sized (monodisperse) distribution have been derived in the literature.
Wladimir Lyra+3 more
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Abstract Results of microanalysis study of NWA 869 meteorite, an ordinary chondrite, where silicates, Fe‐Ni alloys, and troilite are major constituents, are reported. The presented study of microtextures in metallic and sulfide grains provides information on processes occurring from the asteroid's accretion, through the impacts until cooling.
Paulina Skirak+4 more
wiley +1 more source
Oligarchic Growth of Protoplanets in Planetesimal Rings
In the standard planet formation scenario, planetesimals are assumed to form throughout the protoplanetary disk and to be smoothly distributed in the radial direction except for the snowline.
Yuki Kambara, Eiichiro Kokubo
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